GEONAVIGATE / RESOURCES

Oilfield glossary

An illustrated dictionary for the language of the wellsite—from subsurface interpretation to drilling, completions and production.

1,485 terms · 43 subject areas · 128 schematics

Original concise definitions covering oil and gas drilling, completions, production, thermal recovery, geothermal, geosteering and formation evaluation. Each entry links to a primary reference. Definitions and diagrams explain terminology; they do not replace a well program, equipment manual or site procedure.

Compiled by GeoNavigate from the linked references. Edition 5, updated 2026-10-31. Suggest a correction or browse the visual reference.

1485 terms

Geophysics & seismic#

Average seismic velocity

Effective vertical seismic speed from a specified datum to a target, calculated as vertical distance divided by one-way travel time under the stated ray-path assumptions. For a vertical two-way reflection time t, the equivalent average is 2z/t; it is not generally the arithmetic mean of the interval velocities.

Worked example: two layers, travel time and depth

Also called: Average velocity (seismic)

References & related terms

SLB Energy Glossary — average velocity Reference checked 2026-10-28

Related: Interval velocity · Two-way travel time · Depth conversion · Checkshot survey · Root-mean-square velocity

View schematic: Two layers: travel time and depth are different coordinates

Geophysics & seismic#

Depth conversion

Transformation of seismic interpretations from travel-time coordinates into estimated depth using a velocity model and consistent reference datums. The result depends on the velocity information and imaging assumptions; changing the axis label alone does not establish a depth model.

Worked example: two layers, travel time and depth

Also called: Seismic time-to-depth conversion

References & related terms

US EPA — Seismic Reflection Reference checked 2026-10-28

Related: Average seismic velocity · Two-way travel time · Interval velocity · Seismic datum · Depth migration · Checkshot survey

View schematic: Two layers: travel time and depth are different coordinates

Reservoir geology#

Global Boundary Stratotype Section and Point GSSP

An internationally ratified reference point in a specified stratigraphic section that fixes a boundary on the geological time scale. Correlation markers help identify its time-equivalent level in other successions.

Field context A local fossil occurrence or log pick is evidence for correlation, not a new GSSP. Check the ratified reference and supporting markers.

Worked example: a fixed boundary and a revised age

Also called: Golden spike

References & related terms

ICS — Global Boundary Stratotype Sections and Points Reference checked 2026-10-25

Related: Global Standard Stratigraphic Age · Chronostratigraphic unit · Geochronologic unit

View schematic: Boundary definition and numerical calibration

Reservoir geology#

Global Standard Stratigraphic Age GSSA

An internationally agreed numerical age used to define a boundary on the geological time scale, particularly in parts of the Precambrian. Its defining reference is a number rather than a designated point in a stratigraphic section.

Field context Distinguish a defining GSSA from the estimated numerical age of a GSSP. Consult the current ICS chart for the standard assigned to a particular boundary.

Worked example: a fixed boundary and a revised age

References & related terms

ICS Guide — Chronostratigraphic Units, Precambrian subdivision Reference checked 2026-10-25

Additional interpretation reference

Related: Global Boundary Stratotype Section and Point · Geochronologic unit · Radiometric dating

View schematic: Boundary definition and numerical calibration

Reservoir geology#

Graded bedding

A systematic change in grain size through the thickness of a sedimentary bed. Describe the direction and scale of the change before interpreting the depositional process.

Worked example: grading within one bed

Also called: Sedimentary grading

References & related terms

IODP Expedition 400 — Methods: sedimentary structures Reference checked 2026-10-25

Related: Normal grading · Inverse grading · Grain size · Turbidite

View schematic: Normal and inverse sedimentary grading

Reservoir geology#

Normal grading

An upward decrease in grain size within a bed, with coarser particles below finer particles. Upward refers to stratigraphic younging, which need not coincide with present vertical.

Field context Determine stratigraphic way-up separately from present vertical: a normal graded bed fines toward its original top even after overturning. Confirm the depositional interpretation with other indicators before assigning younging.

Worked example: which way is stratigraphic up?

Also called: Normally graded bedding

References & related terms

IODP Expedition 400 — Methods: sedimentary structures Reference checked 2026-10-25

Related: Graded bedding · Inverse grading · Grain size · Turbidite · Younging direction · Overturned bedding

View schematic: Normal and inverse sedimentary grading

Reservoir geology#

Inverse grading

An upward increase in grain size within a bed. The observation describes a texture; it does not by itself identify a unique transport mechanism or depositional environment.

Worked example: grading within one bed

Also called: Reverse grading, Inversely graded bedding

References & related terms

IODP Expedition 400 — Methods: sedimentary structures Reference checked 2026-10-25

Related: Graded bedding · Normal grading · Grain size · Turbidite

View schematic: Normal and inverse sedimentary grading

Reservoir engineering#

Absolute permeability

Rock permeability measured with a single fluid phase occupying its connected pores.

Field context In the single-phase Darcy-flow context, this corresponds to intrinsic permeability of the pore network. Hydraulic conductivity additionally incorporates fluid properties: K = kρg/μ. This comparison assumes unchanged pore geometry and a fully saturated medium.

Worked example: permeability versus hydraulic conductivity

Also called: Intrinsic permeability

References & related terms

SLB Energy Glossary — absolute permeability Reference checked 2026-10-24

Field-context reference

Related: Reservoir · Permeability · Hydraulic conductivity

View schematic: Same pore network, different hydraulic conductivity

Production fluids and facilities#

Absorption

Transfer of a substance into the bulk of another material, such as water vapor entering glycol during gas drying.

References & related terms

SLB Energy Glossary — absorption Reference checked 2026-10-24

Related: Adsorption · Desiccant

Petroleum fluids and properties#

Acid gas

Gas constituent or separated stream, commonly hydrogen sulfide or carbon dioxide, capable of forming acidic water solutions.

References & related terms

SLB Energy Glossary — acid gas Reference checked 2026-10-24

Related: Sour gas · Amine treating

Stimulation#

Acid wash

Acid treatment directed at deposits in the wellbore, perforations, or completion equipment rather than deep formation stimulation.

References & related terms

SLB Energy Glossary — Acid wash Reference checked 2026-10-24

Related: Scale · Acidizing

Geophysics & seismic#

Acoustic impedance

Product of rock bulk density and compressional-wave velocity; contrasts between layers influence seismic reflections.

Field context For a P wave, Z = bulk density × P-wave velocity. Use compatible units: kg/m³ × m/s gives kg/(m²·s). Equal impedance can occur in different lithologies; impedance is not a unique rock identifier. For example, 2000 kg/m³ × 3000 m/s and 2500 kg/m³ × 2400 m/s both give 6 million kg/(m²·s), despite different densities and speeds.

Worked example: different properties, equal impedance

Also called: Seismic impedance

References & related terms

SLB Energy Glossary — acoustic impedance Reference checked 2026-10-30

Field-context reference

Related: Synthetic seismogram · Sonic log · Normal incidence · Reflectivity series

View schematic: Acoustic impedance and seismic reflection

Geophysics & seismic#

Amplitude variation with offset AVO

Change in seismic reflection amplitude with source-receiver separation, analyzed for information about lithology and fluids but subject to nonunique interpretation.

Also called: Amplitude versus offset

References & related terms

SLB Energy Glossary — avo Reference checked 2026-10-24

Related: Acoustic impedance · Synthetic seismogram · Sonic log

Geosteering & modelling#

Anisotropy

Variation of a material property with measurement direction, such as different seismic velocities parallel and perpendicular to bedding.

Field context Name the property and scale: hydraulic anisotropy concerns conductivity, not necessarily seismic velocity or electrical resistivity. Isotropic beds can form an anisotropic layered unit.

Worked example: conductivity along and across layers

References & related terms

SLB Energy Glossary — anisotropy Reference checked 2026-10-24

Field-context reference

Related: Geosteering · Forward modelling · Geophysical inversion · Layered heterogeneity · Equivalent hydraulic conductivity · Isotropy · Hydraulic conductivity tensor

View schematic: Layer-parallel and layer-normal groundwater flow

Reservoir geology#

Anticline

Fold with older beds in its core, commonly forming an upward arch that can create a structural hydrocarbon trap.

Field context Separate fold shape from stratigraphic age: antiform and synform describe closure, whereas anticline and syncline require age evidence. Record the profile orientation before measuring limb angles.

Worked example: fold profile and bed age

References & related terms

SLB Energy Glossary — anticline Reference checked 2026-10-24

Additional interpretation reference

Related: Syncline · Fold · Structural trap · Synform · Interlimb angle · Antiform

View schematic: Fold profile: shape, limb angle and bed age

Geosteering & modelling#

Apparent dip

Inclination of a geological plane seen in a vertical section not aligned with its maximum-dip direction.

Field context Specify the section direction or borehole-coordinate convention. A dip seen along the well direction can differ from maximum geological dip; using the wrong projection changes the interpreted stratigraphic position. For a nonvertical plane, tan(apparent dip) = tan(true dip) × cos(theta), where theta is the horizontal angle from the down-dip direction to the section heading. A negative result means the surface rises along that heading. Two perpendicular signed section slopes of the same planar surface can recover its dip: combine their tangents as orthogonal components, rather than averaging the angles.

Worked example: recover dip from perpendicular sections

References & related terms

SLB Energy Glossary — Apparent dip Reference checked 2026-10-25

Field-context reference

Additional interpretation reference

Related: Formation dip · Strike · Dip direction · Right-hand rule · Vertical exaggeration

View schematic: Strike, dip direction and apparent dip

Hydrogeology & pore systems#

Average linear groundwater velocity

Mean advective groundwater speed estimated as v = q/ne, where q is Darcy flux and ne is effective flow porosity. This averages pore paths and does not include dispersion or solute retardation.

Field context For uniform steady flow, t = L ne/q. State the flow-porosity assumption and test its sensitivity; this time is not a first-arrival or contaminant-breakthrough prediction.

Worked example: flow porosity and travel-time sensitivity

Also called: Seepage velocity, Average pore-water velocity

References & related terms

The Groundwater Project — groundwater flow principles Reference checked 2026-10-29

Related: Hydraulic head · Hydraulic gradient · Darcy flux · Sorption · Sorption distribution coefficient · Retardation factor · Mechanical dispersion · Dispersivity

View schematic: Groundwater head loss and Darcy flux

Survey quality & positioning#

Azimuth AZI

Horizontal direction measured from a stated north reference; true, grid and magnetic north are not interchangeable.

Field context Record whether the heading is magnetic, true or grid referenced. Converting between references requires the applicable declination and convergence conventions.

References & related terms

SLB Energy Glossary — Azimuth Reference checked 2026-10-24

Field-context reference

Related: Measured depth · True vertical depth · Depth reference · Inclination · Dogleg severity · Toolface

View schematic: True, grid and magnetic north

Drilling fluids#

Barite sag

Settling and redistribution of weighting solids that create mud-density differences within the circulating system or well.

Also called: Weighting-material sag

References & related terms

SLB Energy Glossary — sag Reference checked 2026-10-24

Related: Mud weight · Barite · Mud balance

Production chemistry#

Biocide

Chemical treatment used to control microorganisms in oilfield fluids and equipment.

Also called: Bactericide

References & related terms

SLB Energy Glossary — biocide Reference checked 2026-10-24

Related: Produced water

Reservoir geology#

Biostratigraphy

Use of fossils to date and correlate sedimentary intervals and help interpret depositional environments.

Field context Check assemblage consistency and possible reworking before assigning a host-bed age from a fossil occurrence. State whether a reported range is local or compiled across sections; correlation requires an explicit zonal criterion. Reworking is a depositional history; drilling cavings are sample contamination. Do not interpret a mixed fossil assemblage until these possibilities have been considered.

Worked example: reworking versus drilling cavings

References & related terms

SLB Energy Glossary — biostratigraphy Reference checked 2026-10-24

Field-context reference

Additional interpretation reference

Related: Lithology · Stratigraphy · Porosity · Reworked fossil · Fossil disarticulation · Polarity zone · Polarity chron · Fossil time averaging · Death assemblage · Taxon-range zone · Concurrent-range zone · Cavings · Assemblage biozone · Abundance biozone · Lineage biozone · Barren interval

Additional schematic: Fossil reworking and drilling cavings

View schematic: Fossil reworking: two burial histories

Drilling dynamics & BHA#

Bottomhole assembly BHA

Lower drillstring components used to cut, guide, stabilize and measure the borehole.

Field context Record component order, dimensions and sensor positions as well as tool names. Two assemblies carrying similar tools can behave differently because their geometry and stabilization differ.

References & related terms

OSHA / PETEX drilling glossary — B Reference checked 2026-10-24

Field-context reference

Related: Drill pipe · Drill collar · Drill bit

View schematic: The drilling-fluid circulation loop

Well intervention#

Burn shoe

Hollow milling tool used to prepare the outside or top of a fish for retrieval.

Also called: mill shoe, washover shoe

References & related terms

SLB Energy Glossary — Burn shoe Reference checked 2026-10-24

Related: Washover · Overshot

Cementing and casing#

Buttress thread

A casing-connection thread form designed to carry axial load, with sealing dependent on the connection design and fit.

References & related terms

SLB Energy Glossary — Buttress thread Reference checked 2026-10-24

Related: Cementing · Casing

Reservoir geology#

Calcite

Calcium-carbonate mineral that is a major constituent of limestone and a common cement in sedimentary rocks.

Field context Calcite and aragonite share the ideal formula CaCO3 but differ in crystal structure. Calcite identified in a fossil is not by itself proof that the organism originally secreted calcite.

Worked identification: composition versus crystal structure

References & related terms

SLB Energy Glossary — calcite Reference checked 2026-10-24

Additional interpretation reference

Related: Lithology · Stratigraphy · Porosity · Aragonite · Polymorphism

View schematic: Same composition, different mineral structures

Reservoir engineering#

Capillary entry pressure

Threshold pressure difference at which a non-wetting fluid first invades an accessible, initially wetting-fluid-filled pore connection under a specified displacement path. Geometry, interfacial tension and wetting conditions control the threshold.

Field context Check whether a measured throat size is radius or diameter. In the ideal tube model, a 10 μm diameter means r = 5 μm, giving 12 kPa for γ = 0.030 N/m and water-side θ = 0°. Treating that diameter as radius incorrectly gives 6 kPa. Preserve phase order and angle convention when transferring software inputs.

Worked example: radius versus diameter

Also called: Entry capillary pressure

References & related terms

Idaho National Laboratory FALCON — Capillary pressure Reference checked 2026-10-30

Field-context reference

Related: Wettability · Capillary pressure

View schematic: Pore-throat radius and capillary entry

Reservoir engineering#

Capillary pressure

Pressure difference across a fluid interface. Here Pc is non-wetting-phase pressure minus wetting-phase pressure; always state the phase order because sign conventions differ.

Capillary entry: worked pore-throat example

Also called: Pc

References & related terms

Idaho National Laboratory FALCON — Capillary pressure Reference checked 2026-10-25

Related: Wettability · Capillary entry pressure · Drainage displacement · Imbibition · Capillary-pressure hysteresis

View schematic: Pore-throat radius and capillary entry

Cementing and casing#

Casing head

The lower wellhead adapter attached to the first casing string and supporting subsequent wellhead or pressure-control equipment.

Also called: casinghead

References & related terms

SLB Energy Glossary — Casing head Reference checked 2026-10-24

Related: Cementing · Casing

Cementing and casing#

Casing thread

Machined helical connection geometry joining casing components and contributing to structural and pressure integrity.

References & related terms

SLB Energy Glossary — Casing thread Reference checked 2026-10-24

Related: Cementing · Casing

Gas processing and refining#

Catalytic hydrocracking

Conversion of heavier petroleum fractions into lighter products using hydrogen and catalysts.

Also called: Hydrocracking

References & related terms

U.S. EIA Energy Glossary — C Reference checked 2026-10-24

Related: Crude oil · Natural gas liquids

Gas processing and refining#

Catalytic hydrotreating

Hydrogen-and-catalyst treatment of petroleum fractions to improve quality and remove unwanted constituents.

Also called: Hydrotreating

References & related terms

U.S. EIA Energy Glossary — C Reference checked 2026-10-24

Related: Crude oil · Natural gas liquids

Wellsite geology & samples#

Cavings

Fragments detached from the borehole wall rather than newly drilled at the bit; they can contaminate cuttings samples.

Field context Older material falling from an unstable interval can appear with newly drilled cuttings. Do not assign every recovered fragment to the current bit formation; retain the evidence for a mixed sample. Material from an interval penetrated earlier need not be geologically older. In an upright, unfaulted succession, younger fossils can cave from above into a sample collected while drilling older beds. Folded or faulted sections require their own age-order model.

Worked example: reworking versus drilling cavings

References & related terms

SLB Energy Glossary — Cavings Reference checked 2026-10-24

Additional interpretation reference

Related: Cuttings · Lag depth · Reworked fossil · Biostratigraphy

Additional schematic: Fossil reworking and drilling cavings

View schematic: The drilling-fluid circulation loop

Cementing and casing#

Cement head

Surface equipment connected to casing that holds and releases cementing plugs and provides fluid connections.

References & related terms

SLB Energy Glossary — Cement head Reference checked 2026-10-24

Related: Cementing · Casing

Cementing and casing#

Cementing spacer

Engineered viscous fluid placed between drilling fluid and cement to improve displacement and limit contamination.

Also called: spacer fluid, cement spacer

References & related terms

SLB Energy Glossary — Cementing spacer Reference checked 2026-10-24

Related: Cementing · Casing

Geophysics & seismic#

Checkshot survey

Borehole survey measuring travel time from a surface seismic source to receivers at known depths to calibrate time-depth relationships.

Field context Checkshot first arrivals provide source-to-receiver times, not automatically surface-reflection two-way times. Survey geometry, well deviation and seismic reference datum corrections must be reconciled before using the resulting time–depth relationship for a well tie.

Worked example: two layers, travel time and depth

Also called: Check-shot survey

References & related terms

SLB Energy Glossary — check-shot survey Reference checked 2026-10-24

Field-context reference

Related: Acoustic impedance · Synthetic seismogram · Sonic log · Average seismic velocity · Depth conversion

View schematic: Two layers: travel time and depth are different coordinates

Reservoir geology#

Chlorite

Platy green silicate mineral that can occur as pore-lining coatings in sandstone and influence reservoir quality.

Field context Chlorite can belong to an earlier low-grade assemblage or form during later replacement. Report its texture and associated minerals before interpreting metamorphic history.

Worked guide: mineral evidence, isograds and overprints

References & related terms

SLB Energy Glossary — chlorite Reference checked 2026-10-24

Additional interpretation reference

Related: Lithology · Stratigraphy · Porosity · Isograd · Retrograde metamorphism

View schematic: Isograd evidence and a later mineral overprint

Reservoir geology#

Clast imbrication

An overlapping, preferentially inclined arrangement of sedimentary clasts. In the common upstream-dipping fabric, the broad clast surfaces dip against the inferred flow direction; long-axis orientation must be recorded separately.

Field context Average dip azimuths as circular directions, not ordinary numbers. Keep measured dip directions, inferred flow directions and undirected long-axis orientations distinct; a circular mean is not a bedding-restoration calculation.

Worked example: averaging bearings across north

Also called: Pebble imbrication, Imbricated clasts

References & related terms

Brenna et al. (2024) — Imbrication fabric and gravel transport processes Reference checked 2026-10-29

Field-context reference

Related: Paleocurrent · Conglomerate · Cross-bedding

View schematic: Clast imbrication and inferred flow

Reservoir geology#

Closed isotopic system

A mineral or rock domain that has neither gained nor lost the relevant parent or daughter isotopes over the interval being dated, apart from internal radioactive decay. Closure is specific to an isotope system and geological history.

Field context A lower retained daughter/parent ratio can reflect daughter loss rather than a younger formation event. The worked loss example holds parent constant; it is not a universal correction for disturbed samples.

Worked example: daughter loss and apparent age

References & related terms

USGS — Radiogenic Isotopes Reference checked 2026-10-29

Field-context reference

Additional interpretation reference

Related: Radiometric dating · Parent isotope · Daughter isotope · Half-life · Radiogenic isotope · Thermochronology · Closure temperature

View schematic: Radioactive decay in a closed teaching system

Production chemistry#

Coalescence

Merging of small dispersed liquid droplets into larger droplets, which can promote phase separation.

References & related terms

SLB Energy Glossary — coalescence Reference checked 2026-10-24

Related: Emulsion · Scale

Thermal operations#

Cogeneration CHP

Producing useful heat and electricity from a shared energy source, such as at a steam-intensive oil-sands facility.

Also called: combined heat and power

References & related terms

Government of Alberta — Oil sands glossary Reference checked 2026-10-24

Related: Thermal recovery

Reservoir geology#

Compaction

Reduction of sediment volume as grains pack more closely or deform, commonly decreasing pore space during burial.

Field context A pore-pressure decline can increase effective stress even without additional burial. Predicting deformation also requires compressibility, stress history and drainage times; the stress change alone does not give a settlement.

Effective stress and compaction: worked example

References & related terms

SLB Energy Glossary — Compaction Reference checked 2026-10-24

Field-context reference

Related: Diagenesis · Porosity · Lithification · Effective stress · Pore-water pressure · Total vertical stress · Preconsolidation stress · Mechanical compaction · Pressure solution

View schematic: Effective stress during pore-pressure decline

Field personnel#

Company representative

Operator's onsite representative responsible for coordinating and overseeing wellsite operations.

Also called: Company man, Wellsite supervisor

References & related terms

SLB Energy Glossary — company man Reference checked 2026-10-24

Related: Toolpusher · Derrickhand · Tour

Wellsite geology & samples#

Conchoidal fracture

A mineral or glass breakage texture with curved, shell-like surfaces rather than repeated planar cleavage. Quartz commonly shows this texture, but the texture alone does not establish mineral identity.

Mineral identification: cleavage, fracture and parting

Also called: Shell-like fracture

References & related terms

Oxford University Museum — Cleavage and fracture Reference checked 2026-10-24

Related: Mineral fracture · Mineral parting

View schematic: Cleavage directions versus fracture

Health, safety and environment#

Confined-space attendant

Person stationed outside a confined space to monitor entrants and coordinate assistance.

Also called: safety watch, standby person

References & related terms

CCOHS — Confined Space Program Reference checked 2026-10-24

Related: Confined space · Risk assessment

Reservoir geology#

Conglomerate CGL

Sedimentary rock containing abundant rounded gravel-sized fragments within a finer matrix or cement.

Field context Describe clast orientation separately from roundness and sorting. An imbricated fabric can constrain flow interpretation, but a conglomerate name alone does not identify the transport process.

From grain shape to clast fabric

References & related terms

USGS — Lithologic classification of geologic map units Reference checked 2026-10-24

Field-context reference

Related: Bubblepoint pressure · Fault · Fluid saturation · Formation dip · Clast imbrication · Paleocurrent

View schematic: Clast imbrication and inferred flow

Reservoir engineering#

Contact angle

Angle where two fluid phases meet a solid surface, measured through a specified phase to characterize wetting.

Field context For a cylindrical, water-wet throat, entry pressure scales with interfacial tension and the cosine of the contact angle measured through water, and inversely with throat radius. A larger pore body does not remove a narrow connecting throat. At one ideal flat contact, water-side and oil-side angles sum to 180°. Record which phase advances or recedes; a single smooth-surface measurement is not a complete rock wettability description.

Worked example: supplementary contact angles

References & related terms

SLB Energy Glossary — contact angle Reference checked 2026-10-29

Additional interpretation reference

Related: Reservoir · Permeability · Capillary pressure · Capillary entry pressure

Additional schematic: One interface, two phase-side angles

View schematic: Pore-throat radius and capillary entry

Mudlogging & samples#

Core analysis

Laboratory evaluation of recovered rock to measure properties such as porosity, permeability, saturation and fabric.

References & related terms

SLB — Defining Coring Reference checked 2026-10-24

Related: Core · Sidewall core · Porosity

Reservoir geology#

Cross-bedding

Sets of inclined internal layers within a bed, commonly produced as ripples or dunes migrate.

Field context Terminology varies: dune-scale cross-stratification is commonly called cross-bedding and ripple-scale structures cross-lamination. Identify the set boundary that truncates older laminae before inferring stratigraphic way-up; internal lamina dip alone is insufficient.

Worked example: cross-bed truncation and way-up

References & related terms

Texas A&M Ocean Drilling Program — Sedimentary rock classification Reference checked 2026-10-28

Additional interpretation reference

Related: Facies · Depositional environment · Current ripple · Wave ripple · Younging direction · Overturned bedding · Lamination

Additional schematic: Cross-bed truncation and stratigraphic way-up

View schematic: Ripple profiles: current direction and oscillation axis

Field reporting#

Daily drilling report DDR

Time-bounded record of well operations, progress and notable conditions for communication between the rig and office.

References & related terms

OSHA / PETEX — Drilling glossary D Reference checked 2026-10-24

Related: Mud logging

Hydrogeology & pore systems#

Darcy flux

Volumetric discharge divided by the bulk cross-sectional area normal to flow: q = Q/A. For one-dimensional saturated Darcy flow, q = −K dh/dx. Its units are length per time, but it is not the velocity within connected pores.

Field context Use the bulk area for q = Q/A; dividing by flow porosity gives an average advective speed, not a local pore-channel speed.

Worked example: flow porosity and travel-time sensitivity

Also called: Specific discharge, Darcy velocity

References & related terms

The Groundwater Project — groundwater flow principles Reference checked 2026-10-29

Related: Hydraulic head · Hydraulic gradient · Average linear groundwater velocity

View schematic: Groundwater head loss and Darcy flux

Reservoir geology#

Daughter isotope

An isotope produced by radioactive decay of a parent isotope.

Field context Measured daughter atoms can include both initial and radiogenic components. Treating all daughter atoms as decay products can bias an age.

Radiometric dating: half-life and age interpretation

References & related terms

Minnesota Geological Survey — Geologic Time Reference checked 2026-10-25

Additional interpretation reference

Related: Half-life · Parent isotope · Radiometric dating · Radiogenic isotope · Closed isotopic system

View schematic: Radioactive decay in a closed teaching system

Production chemistry#

Defoamer

Chemical additive used to break foam and help trapped gas escape from a liquid.

Also called: Antifoam, Foam breaker

References & related terms

SLB Energy Glossary — defoamer Reference checked 2026-10-24

Related: Surfactant · Emulsion

Petroleum fluids and properties#

Density

Mass per unit volume of a material or fluid.

Field context State the mass and volume basis, units and material condition. A heavier specimen is not necessarily denser if its volume is larger.

Worked example: density, equal volume and specific gravity

References & related terms

SLB Energy Glossary — density Reference checked 2026-10-29

Additional interpretation reference

Related: Specific gravity · API gravity

View schematic: Density and specific gravity: equal-volume comparison

Geosteering & modelling#

Depth matching

Alignment of logs, cores or other well data to a consistent depth reference before comparison or integration.

Field context A visually improved alignment should retain its reference curve, method and applied shifts. Keep acquisition depths available so a later reviewer can reproduce or challenge the match.

References & related terms

SLB Energy Glossary — depth matching Reference checked 2026-10-24

Related: Porosity · Resistivity log · Wireline logging

Petrophysics & log interpretation#

Depth of investigation DOI

Characteristic distance into the formation contributing to a tool measurement; its meaning depends on the response and stated signal fraction.

Field context The quoted distance depends on how sensitivity is defined and on formation conditions. It should not be interpreted as a sharp boundary beyond which a tool has zero response.

References & related terms

SLB Energy Glossary — depth of investigation Reference checked 2026-10-24

Related: Porosity · Resistivity log · Wireline logging

Reservoir geology#

Diagenesis

Physical, chemical and biological changes to sediment after deposition, generally below metamorphic conditions. These changes can alter reservoir quality.

References & related terms

SLB Energy Glossary — Diagenesis Reference checked 2026-10-24

Related: Compaction · Lithification · Geological cement · Mineral replacement · Pseudomorph · Mechanical compaction · Pressure solution · Isotope delta · Isotope fractionation

View schematic: Replacement with an inherited outline

Geosteering & modelling#

Dip direction

Compass bearing of the steepest downward line in an inclined geological plane. It is perpendicular to strike and identifies which way the plane descends; it is an azimuth, not the dip angle.

Worked example: strike and apparent dip

Also called: Dip azimuth

References & related terms

University of Alberta — Orientation of structures Reference checked 2026-10-25

Related: Strike · Formation dip · Apparent dip · Right-hand rule

View schematic: Strike, dip direction and apparent dip

Survey quality & positioning#

Directional survey

Measurement of wellbore inclination and azimuth at a specified depth, used to reconstruct its path.

Field context A station measures direction at a location. The continuous path shown between stations is calculated, so survey spacing and the reconstruction method affect what small-scale bends can be resolved.

Also called: Deviation survey

References & related terms

SLB Energy Glossary — directional survey Reference checked 2026-10-24

Related: Directional drilling · Inclination · Azimuth

View schematic: A survey is sampled; the path is reconstructed

Directional drilling & trajectory#

Dogleg severity DLS

Change in wellbore direction per unit length, commonly expressed as degrees per 30 m or 100 ft.

Field context Build rate describes inclination change; dogleg severity includes both inclination and azimuth change. Values normalized per 30 m and per 100 ft are close but not numerically identical.

Also called: DLS

References & related terms

SLB — Directional drilling practices Reference checked 2026-10-24

Field-context reference

Related: Measured depth · True vertical depth · Depth reference · Inclination · Azimuth · Keyseat

View schematic: Well geometry: along-hole and vertical depth

Reservoir geology#

Downlap

Termination of inclined strata against an underlying surface with a shallower apparent dip.

Field context Read the termination relative to the lower bounding surface and original depositional geometry. In the standard usage, onlap ends updip and downlap ends downdip; present apparent dip alone may be misleading after deformation.

Worked interpretation: reflection terminations and uncertainty

References & related terms

SLB Energy Glossary — downlap Reference checked 2026-10-24

Additional interpretation reference

Related: Onlap · Progradation · Retrogradation · Sequence stratigraphy · Baselap · Toplap

View schematic: Reflection terminations: identify the bounding surface first

Reservoir engineering#

Drainage displacement

Increase of nonwetting-phase saturation as that phase enters a porous rock.

Field context Identify the wetting fluid before classifying displacement. Track saturation reversals when comparing capillary-pressure data; the worked example is conceptual, not a field calibration.

Worked example: saturation and displacement history

References & related terms

SLB Energy Glossary — drainage Reference checked 2026-10-24

Related: Reservoir · Permeability · Capillary-pressure hysteresis · Wettability · Imbibition

View schematic: Same saturation, different displacement history

Petrophysics & log interpretation#

Effective porosity

Interconnected pore fraction available for fluid flow; petrophysical conventions commonly exclude clay-bound water, so the interpretation basis should be stated.

Field context State the measurement convention: dry-core connected porosity excludes isolated pores; a common log convention subtracts clay-bound water from total porosity. These are not interchangeable corrections. Retain sample preparation, method and bulk-volume basis with the result.

Worked example: porosity measurement conventions

References & related terms

SLB Energy Glossary — effective porosity Reference checked 2026-10-29

Related: Total porosity · Primary porosity · Secondary porosity · Porosity · Sorption · Sorption distribution coefficient · Retardation factor

Additional schematic: Porosity and connected flow

View schematic: Water movement and reversible sorption

Reservoir geology#

Effective stress

Stress acting on the solid framework of a porous material. For a saturated soil under the Terzaghi convention, effective normal stress equals total normal stress minus pore-water pressure; compression is positive.

Field context When a falling water table reduces the weight of overlying sediment, total stress also changes. At a point that remains saturated, use Δσ′v = Δσv − Δu rather than treating the pressure decline alone as the effective-stress increase.

Worked example: falling water table and changing load

Also called: Intergranular stress

References & related terms

UWE GeotechniCAL — Stress in the ground Reference checked 2026-10-25

Related: Pore-water pressure · Total vertical stress · Preconsolidation stress · Compaction

View schematic: Effective stress during pore-pressure decline

Production and artificial lift#

Electric submersible progressing cavity pump ESPCP

A progressing-cavity pump powered by a downhole electric motor rather than a surface-driven rod string.

Also called: electric submersible progressive cavity pump

References & related terms

SLB — ESPCP Systems Reference checked 2026-10-24

Related: Progressing cavity pump · Artificial lift

Petrophysics & log interpretation#

Electrical anisotropy

Directional variation of electrical resistivity, commonly expressed as a difference between horizontal and vertical formation resistivity.

Field context For continuous horizontal isotropic layers in ideal DC experiments, resistivity parallel to bedding is the thickness-weighted harmonic mean; normal resistivity is the thickness-weighted arithmetic mean. Name the axes and scale. These equivalent material values are not automatically apparent resistivities measured by a surface array or logging tool, and do not determine hydraulic conductivity.

Worked example: electrical versus hydraulic anisotropy

References & related terms

SLB Energy Glossary — electrical anisotropy Reference checked 2026-10-24

Additional interpretation reference

Related: Propagation resistivity · Attenuation resistivity · Phase-shift resistivity · Anisotropy · Layered heterogeneity

View schematic: Electrical resistivity along and across layers

Health, safety and environment#

Energy-isolating device

Mechanical device that physically blocks energy transmission, such as a disconnect or isolating valve.

References & related terms

CCOHS — Lockout/Tag out Reference checked 2026-10-24

Related: Hazardous energy · Stored energy

Reservoir engineering#

Enhanced oil recovery EOR

Processes that change fluid or rock-fluid behavior to recover additional oil, including thermal, chemical, and miscible methods.

Also called: tertiary recovery

References & related terms

SLB Energy Glossary — enhanced oil recovery Reference checked 2026-10-24

Related: Reservoir · Permeability

Reservoir geology#

Fault

Fracture or fracture zone across which rock bodies have moved relative to one another.

Field guide: fault core, damage zone and slickenlines

References & related terms

SLB Energy Glossary — Fault Reference checked 2026-10-24

Related: Formation dip · Isopach · Geosteering · Sandstone · Siltstone · Shale · Fault core · Fault damage zone · Slickenline · Ductile shear zone · Mylonite · Fault separation · Net slip · Piercing point

View schematic: Fault-zone architecture and slip-direction evidence

Reservoir geology#

Feldspar

Group of common silicate minerals present in many sandstones and crystalline rocks; alteration can produce clay minerals.

Field context In ideal plagioclase, replacing Na+ with Ca2+ is balanced by replacing Si4+ with Al3+: both paired contributions total +5. An30 denotes 30 mole percent anorthite component, not 30 percent calcium by mass.

Worked example: plagioclase charge balance

References & related terms

SLB Energy Glossary — feldspar Reference checked 2026-10-24

Field-context reference

Related: Lithology · Stratigraphy · Porosity · Crystal twinning · Polysynthetic twinning · Microcline · Mineral–melt partition coefficient · Compatible element · Incompatible element · Mineral exsolution · Perthite · Compositional zoning · Oscillatory zoning

Additional schematic: Plagioclase coupled substitution

View schematic: Feldspar twin patterns and an unresolved grain

Well intervention#

Fishing

Operations to recover equipment or material left unintentionally in the well, using tools suited to the object and hole conditions.

References & related terms

SLB Energy Glossary — Fishing Reference checked 2026-10-24

Related: Fish · Fishing tool · Jar

Mudlogging & samples#

Flame ionization detector FID

Instrument that measures an electrical response from hydrocarbons burning in a hydrogen flame; used for total-gas detection.

References & related terms

SLB — Defining Mud Logging Reference checked 2026-10-24

Related: Mud logging · Gas show · Cuttings

Field personnel#

Floorhand

Rig-crew member who handles tubular connections and supports rig-floor equipment operation and maintenance.

Also called: Roughneck, Floor hand

References & related terms

SLB Energy Glossary — roughneck Reference checked 2026-10-24

Related: Toolpusher · Derrickhand · Tour

Wellsite geology & samples#

Fluorescence

Visible light emitted under ultraviolet illumination; hydrocarbon interpretation must consider mineral and drilling-fluid fluorescence.

References & related terms

SLB — Defining Mud Logging Reference checked 2026-10-24

Related: Mud logging · Gas show · Cuttings

Reservoir geology#

Fold

Bend in originally straighter rock layers produced by deformation.

Field context A hinge line, an intersection lineation and a stretching lineation are not interchangeable. Compare orientations and fabric relationships before using any lineation as a fold-axis proxy.

Worked example: separate lineation mechanisms

References & related terms

SLB Energy Glossary — fold Reference checked 2026-10-24

Related: Anticline · Syncline · Structural trap · Lineation · Intersection lineation · Crenulation lineation · Stretching lineation · Flexural slip · Flexural flow

View schematic: Lineation mechanisms and interpretation checks

Reservoir geology#

Formation

Primary lithostratigraphic unit: a distinguishable, mappable body of rock defined by lithological characteristics.

Field context A lithological boundary is not automatically a time surface. Track the rock pick and its age interpretation separately.

Worked example: rock boundary versus time surface

References & related terms

International Commission on Stratigraphy — Lithostratigraphic units Reference checked 2026-10-25

Additional interpretation reference

Related: Member · Bed · Lithology · Unconformity · Stratigraphy · Stratigraphic horizon · Diachronous · Isochronous

View schematic: A rock boundary can cross time surfaces

Geosteering & modelling#

Formation dip

Inclination of a geological surface from horizontal, specified together with the direction of maximum downward slope.

Field context For a planar bed, maximum true dip is measured perpendicular to strike. A single apparent dip from one section does not determine the full three-dimensional attitude. True dip is the maximum inclination below horizontal. It is measured perpendicular to strike; an oblique section generally shows a smaller angle.

Worked example: strike and apparent dip

Also called: Dip, True dip

References & related terms

SLB Energy Glossary — Formation dip Reference checked 2026-10-25

Additional interpretation reference

Related: Fault · Isopach · Geosteering · Sandstone · Siltstone · Shale · Dip direction · Right-hand rule

View schematic: Strike, dip direction and apparent dip

Geosteering & modelling#

Forward modelling

Calculation of the measurements a sensor should produce for a specified subsurface model, tool configuration and environment.

Field context The predicted result belongs to a specified sensor, geological model and environment. A generic curve-shape match is not automatically a physical electromagnetic forward model.

Also called: Forward modeling

References & related terms

SLB Energy Glossary — forward modeling Reference checked 2026-10-24

Related: Geophysical inversion · Subsurface model · Geosteering

Reservoir geology#

Fossil

Preserved remains or evidence of past organisms, such as shells, casts, tracks or burrows.

Field context Record preservation and host sediment separately; an older fossil can be redeposited into a younger bed.

Fossil preservation and reworking: worked interpretation

References & related terms

SLB Energy Glossary — fossil Reference checked 2026-10-24

Field-context reference

Related: Lithology · Stratigraphy · Porosity · Reworked fossil · Fossil disarticulation

View schematic: Fossil reworking: two burial histories

Gas processing and refining#

Fractionation

Separation of a hydrocarbon mixture into product fractions, such as ethane, propane, and butanes.

Field context This entry concerns product separation in processing. Isotope fractionation describes redistribution of isotopes and is a separate concept.

References & related terms

U.S. EIA Energy Glossary — F Reference checked 2026-10-24

Related: Crude oil · Natural gas liquids · Isotope fractionation

Cementing and casing#

Free water in cement

Water that separates from a cement slurry rather than remaining uniformly incorporated, potentially leaving unwanted channels.

Also called: cement free water

References & related terms

SLB Energy Glossary — Free water in cement Reference checked 2026-10-24

Related: Cementing · Casing

Wellsite geology & samples#

Gas chromatography GC

Separation and measurement of individual gas components, allowing composition to be evaluated alongside total-gas readings.

References & related terms

SLB — Defining Mud Logging Reference checked 2026-10-24

Related: Mud logging · Gas show · Cuttings

Production fluids and facilities#

Gas-lift mandrel

Tubing-string component supporting a gas-lift valve and providing its annulus-to-tubing flow passage.

References & related terms

SLB Energy Glossary — gas-lift mandrel Reference checked 2026-10-24

Related: Gas lift

Production fluids and facilities#

Gas-lift valve

Downhole valve controlling admission of lift gas from the annulus into production tubing.

References & related terms

SLB Energy Glossary — gas-lift valve Reference checked 2026-10-24

Related: Gas lift

Production fluids and facilities#

Gate valve

Isolation valve using a sliding slab or wedge across the flow passage.

References & related terms

SLB Energy Glossary — gate valve Reference checked 2026-10-24

Related: Manifold

Geosteering & modelling#

Geophysical inversion

Mathematical estimation of a subsurface model consistent with measured data and stated assumptions; a fit does not guarantee a unique solution.

Field context Several models may fit the same measurements. Report the assumed geometry, available data and uncertainty rather than treating the fitted model as a direct image of the earth.

Also called: Inversion, Inverse problem

References & related terms

SLB Energy Glossary — inversion Reference checked 2026-10-24

Related: Geosteering · Forward modelling

Reservoir geology#

Grain roundness

Degree to which a grain’s corners and edges are smoothed; distinct from its overall shape or sphericity.

Field context Assess edge and corner curvature separately from overall grain proportions. A two-dimensional view can obscure three-dimensional form; breakage during drilling and preparation may introduce fresh angular surfaces.

Grain size and texture: worked examples

Also called: Roundness

References & related terms

Geological Survey of India — Sedimentary rock textures Reference checked 2026-10-24

Additional interpretation reference

Related: Sorting · Grain size · Phi scale · Grain sphericity

View schematic: Grain size, sorting and grain shape

Reservoir geology#

Grain size

Dimensions of sediment particles, described using a stated size scale; size classes should not be inferred solely from rock colour.

Field context State the size scale and measurement method. A sieve aperture, microscope section and laser-derived equivalent diameter need not give identical distributions. Phi increases as diameter decreases.

Grain size and texture: worked examples

References & related terms

Geological Survey of India — Sedimentary rock textures Reference checked 2026-10-24

Additional interpretation reference

Related: Sorting · Grain roundness · Sandstone · Matrix · Phi scale · Grain sphericity · Median grain size · Sieve analysis

View schematic: Grain size, sorting and grain shape

Reservoir geology#

Grain sphericity

Degree to which the three-dimensional form of a particle approaches a sphere. Sphericity concerns overall proportions, whereas roundness concerns smoothing of corners and edges; a rounded elongated grain can have low sphericity.

Field context A circular silhouette in one view does not establish a spherical three-dimensional grain. Record orthogonal dimensions or additional views; keep any axis ratio distinct from a named sphericity index and from corner roundness.

Worked example: a circular view can hide flattening

Also called: Sphericity

References & related terms

Open University — sediment texture Reference checked 2026-10-31

Related: Grain size · Sorting · Grain roundness

View schematic: A circular view can hide a flattened grain

Completions#

Gravel-pack screen

A downhole filter assembly that supports the placed gravel and helps maintain a production flow path.

Also called: sand screen

References & related terms

SLB — Gravel-pack screen Reference checked 2026-10-24

Related: Sand control · Gravel pack

Reservoir geology#

Half-life

The time required for half the atoms of a radioactive isotope to decay.

Field context Each equal half-life removes half of the remaining parent population, not half of the original population. After three half-lives, one eighth remains. With 75% of the original parent remaining in a closed system, elapsed time is log₂(1/0.75) ≈ 0.415 half-lives; linear interpolation between 100% and 50% gives the wrong time.

Worked example: a fraction of a half-life

References & related terms

Minnesota Geological Survey — Geologic Time Reference checked 2026-10-30

Field-context reference

Additional interpretation reference

Related: Parent isotope · Daughter isotope · Radiometric dating · Radiogenic isotope · Closed isotopic system

View schematic: Radioactive decay in a closed teaching system

Geosteering & modelling#

Heterogeneity

Variation of rock properties from one location to another within a formation or reservoir.

Field context Heterogeneity describes changes between locations; anisotropy describes changes with direction. A layered unit can have both, depending on the observation scale.

Worked example: conductivity along and across layers

References & related terms

SLB Energy Glossary — heterogeneity Reference checked 2026-10-24

Field-context reference

Related: Geostatistics · Kriging · Variogram · Layered heterogeneity · Equivalent hydraulic conductivity

View schematic: Layer-parallel and layer-normal groundwater flow

Drilling parameters#

Hook load HKLD

Load supported by the rig hook, affected by suspended equipment, buoyancy, friction and movement. The measurement reference should be stated.

Also called: Hookload

References & related terms

SLB Energy Glossary — Hook load Reference checked 2026-10-24

Related: Weight on bit · Travelling block

Hydrogeology & pore systems#

Hydraulic conductivity

Proportionality between specific discharge and hydraulic gradient for a specified porous medium and fluid. Saturated conductivity has units of length per time and depends on pore geometry, fluid density and dynamic viscosity.

Field context Conductivity has velocity units but is not pore-water travel speed. For fixed pore geometry and density, doubling dynamic viscosity halves K. State the fluid, temperature and test direction; the worked example uses a scalar conductivity.

Worked example: permeability versus hydraulic conductivity

Also called: Coefficient of permeability

References & related terms

The Groundwater Project — hydraulic conductivity and intrinsic permeability Reference checked 2026-10-25

Related: Permeability · Absolute permeability · Transmissivity · Layered heterogeneity · Equivalent hydraulic conductivity · Aquitard · Vertical leakance · Kinematic viscosity

View schematic: Same pore network, different hydraulic conductivity

Hydrogeology & pore systems#

Hydraulic gradient

Change in hydraulic head per unit distance. In coordinate x, dh/dx is signed; flow is toward lower head. A positive head-loss magnitude divided by flow-path length is often reported as i. The gradient is dimensionless.

Field context Convert water-level depths to a common elevation datum before calculating a gradient. Two wells constrain a directional difference, not a unique horizontal flow direction; verify hydraulic connection and comparable observation times.

Worked example: depth to water versus head

References & related terms

The Groundwater Project — groundwater flow principles Reference checked 2026-10-24

Field-context reference

Related: Hydraulic head · Darcy flux · Average linear groundwater velocity · Isotropy · Hydraulic conductivity tensor · Vertical hydraulic gradient · Piezometer

Additional schematic: Water-level depth versus hydraulic head

View schematic: Groundwater head loss and Darcy flux

Hydrogeology & pore systems#

Hydraulic head

Mechanical energy per unit weight of water, expressed as a length relative to a datum. With negligible velocity head, h = z + p/(ρg): elevation head plus pressure head. Compare measurements using compatible datums and fluid-density assumptions.

Field context For a nonflowing observation well, subtract vertical depth to water from the surveyed measuring-point elevation. A deeper water-level reading can still represent higher head when casing elevations differ.

Worked example: depth to water versus head

References & related terms

The Groundwater Project — groundwater flow principles Reference checked 2026-10-24

Field-context reference

Related: Hydraulic gradient · Darcy flux · Average linear groundwater velocity

Additional schematic: Water-level depth versus hydraulic head

View schematic: Groundwater head loss and Darcy flux

Wellsite geology & samples#

Hydrocarbon show

Observed indication of hydrocarbons in samples or measurements; interpretation requires checking origin, contamination and supporting evidence.

Also called: Show

References & related terms

SLB Energy Glossary — Hydrocarbon show Reference checked 2026-10-24

Related: Oil show · Gas show

Reservoir engineering#

Imbibition

Increase of the wetting-phase saturation as that phase enters a porous rock.

Field context Identify the wetting fluid before classifying displacement. Track saturation reversals when comparing capillary-pressure data; the worked example is conceptual, not a field calibration.

Worked example: saturation and displacement history

References & related terms

SLB Energy Glossary — imbibition Reference checked 2026-10-24

Related: Reservoir · Permeability · Capillary-pressure hysteresis · Wettability · Drainage displacement

View schematic: Same saturation, different displacement history

Survey quality & positioning#

In-field referencing IFR

Site-specific refinement of the geomagnetic reference used for magnetic surveying, including local crustal-field information. It supplements a global model rather than correcting every possible downhole measurement error.

Also called: IFR1

References & related terms

British Geological Survey — directional drilling services Reference checked 2026-10-24

Related: Directional survey · Measured depth · Azimuth

View schematic: Well geometry: along-hole and vertical depth

Survey quality & positioning#

Inclination INC

Angle of the well trajectory from vertical: 0° is vertically downward and 90° is horizontal.

Field context Inclination describes departure from vertical, not compass heading. Near-vertical azimuth and high-side orientation can be poorly resolved even when the inclination itself appears stable.

References & related terms

SLB Energy Glossary — Inclination Reference checked 2026-10-24

Related: Measured depth · True vertical depth · Depth reference · Azimuth · Dogleg severity

View schematic: Well geometry: along-hole and vertical depth

Survey quality & positioning#

Interpolated in-field referencing IFR2

Geomagnetic referencing that combines a local field model with time-varying observations to estimate the field during drilling. It addresses external temporal variation as well as the established site reference.

Also called: IIFR

References & related terms

British Geological Survey — directional drilling services Reference checked 2026-10-24

Related: Directional survey · Measured depth · Azimuth

View schematic: Well geometry: along-hole and vertical depth

Geophysics & seismic#

Interval velocity

Seismic-wave velocity within a particular rock interval, rather than an average through the entire overlying section.

Field context In a horizontal, vertically traversed interval, thickness is interval velocity multiplied by the interval one-way travel time. Use half the interval two-way time, not half the cumulative time to its base. Average and RMS velocities answer different questions. When deriving velocity from two boundary times, evaluate their difference and correlated timing errors; a shared time shift cancels.

Worked example: two layers, travel time and depth

References & related terms

SLB Energy Glossary — interval velocity Reference checked 2026-10-29

Field-context reference

Related: Acoustic impedance · Synthetic seismogram · Sonic log · Average seismic velocity · Depth conversion

View schematic: Two layers: travel time and depth are different coordinates

Reservoir engineering#

Irreducible water saturation Swirr

Lowest water fraction retained in a rock sample under a specified displacement pressure or centrifuge condition.

Also called: irreducible water

References & related terms

SLB Energy Glossary — irreducible water Reference checked 2026-10-24

Related: Reservoir · Permeability

Depth & surveys#

Isochore

Contour joining equal true vertical thickness; an isochore map differs from a true-stratigraphic-thickness isopach map.

Field context State the thickness convention in the map legend. Subtracting top and base depths at one XY location gives vertical thickness, not automatically normal thickness. In two locally planar examples with TST 10 m, TVT is 10 m at 0° dip but 20 m at 60° dip; the larger vertical interval alone does not demonstrate stratigraphic thickening.

Worked example: isopach versus isochore

References & related terms

SLB Energy Glossary — Isochore Reference checked 2026-10-28

Related: True vertical thickness · Isopach

View schematic: Bedding dip and thickness

Reservoir geology#

Isopach

Line connecting equal true stratigraphic thickness; an isopach map shows how unit thickness varies spatially.

Field context State the thickness convention in the map legend. Subtracting top and base depths at one XY location gives vertical thickness, not automatically normal thickness. In two locally planar examples with TST 10 m, TVT is 10 m at 0° dip but 20 m at 60° dip; the larger vertical interval alone does not demonstrate stratigraphic thickening.

Worked example: isopach versus isochore

References & related terms

SLB Energy Glossary — Isopach Reference checked 2026-10-28

Related: Formation dip · Fault · Geosteering · True stratigraphic thickness · Isochore

View schematic: Bedding dip and thickness

Health, safety and environment#

Job safety analysis JSA

Task-by-task review identifying hazards and the measures needed to control them.

Also called: job hazard analysis, JHA

References & related terms

CCOHS — Job Safety Analysis Reference checked 2026-10-24

Related: Risk assessment · Hazard control

Wellsite geology & samples#

Lag depth

Estimated source depth assigned to returned cuttings or gas after correcting for transport delay; mixing and cavings can blur that assignment.

References & related terms

IODP Expedition 348 — Methods Reference checked 2026-10-24

Related: Lag time · Cavings · Cuttings · Gas show

Wellsite geology & samples#

Lag time

Transport delay between a downhole event or sample origin and its arrival at the surface observation point; specify the path considered.

Field context Distinguish bottom-to-surface transport from a complete circulation cycle. A time correction alone is inadequate unless the drilling-depth and circulation histories are also known.

Also called: Cuttings transport lag

References & related terms

SLB Energy Glossary — Lag time Reference checked 2026-10-24

Related: Lag depth · Cuttings · Mud logging · Connection gas

View schematic: The drilling-fluid circulation loop

Reservoir geology#

Lamination

Fine-scale layering within a sedimentary bed, reflecting changes during deposition or subsequent modification.

Field context Measure layer thickness normal to its boundaries. A common convention separates laminae below 1 cm from thicker beds; record the convention and actual measurement. Apparent width on an oblique core face is not true thickness.

Worked example: apparent versus true layer thickness

References & related terms

Texas A&M Ocean Drilling Program — Sedimentary rock classification Reference checked 2026-10-28

Additional interpretation reference

Related: Facies · Depositional environment · Current ripple · Wave ripple · Flaser bedding · Lenticular bedding · Bedding · Cross-bedding · Fissility

Additional schematic: Bedding dip and thickness

View schematic: Ripple profiles: current direction and oscillation axis

Reservoir geology#

Lithostratigraphy

Subdivision and correlation of strata based on rock characteristics rather than directly on age.

Field context A lithological boundary is not automatically a time surface. Track the rock pick and its age interpretation separately.

Worked example: rock boundary versus time surface

References & related terms

SLB Energy Glossary — lithostratigraphy Reference checked 2026-10-25

Additional interpretation reference

Related: Lithology · Stratigraphy · Porosity · Diachronous · Isochronous

View schematic: A rock boundary can cross time surfaces

MWD, LWD & telemetry#

Logging while drilling LWD

Measuring formation properties with tools in the bottomhole assembly while the well is being drilled.

Field context Measurement depth, sensor distance behind the bit and telemetry arrival time are separate references. Align them before treating a received log change as the formation at the current bit position.

References & related terms

SLB Energy Glossary — Logging while drilling Reference checked 2026-10-24

Field-context reference

Related: Measurement while drilling · Gamma ray log · Wireline logging · Log correlation

Production fluids and facilities#

Manifold

Assembly of connected pipes and valves distributing, collecting, or controlling fluid streams.

References & related terms

SLB Energy Glossary — manifold Reference checked 2026-10-24

Related: Header · Gate valve

Drilling fluids#

Marsh funnel

Field device measuring the time for a specified fluid volume to drain through an orifice; it provides an empirical flow-time check.

References & related terms

SLB Energy Glossary — Marsh funnel Reference checked 2026-10-24

Related: Viscosity · Rheology

Reservoir geology#

Maximum flooding surface MFS

Stratigraphic surface marking the greatest landward extent of marine flooding within a depositional sequence.

Field context This designation needs sequence-scale stacking and correlation context. An individual flooding contact or a high gamma-ray value does not by itself establish maximum flooding.

Worked example: flooding surfaces and parasequence evidence

References & related terms

SLB Energy Glossary — maximum flooding surface Reference checked 2026-10-28

Additional interpretation reference

Related: Lithology · Stratigraphy · Porosity · Marine flooding surface · Parasequence · Facies

View schematic: Parasequence boundaries and evidence

Wellsite geology & samples#

Mineral cleavage

The tendency of a mineral to split along particular crystallographic planes of relatively weak bonding. Count distinct plane orientations, not the total number of parallel faces; mineral cleavage is different from bedding or cleavage of a rock.

Field context Several parallel surfaces represent one cleavage direction. Record the number of distinct directions and their angles; growth faces alone do not prove cleavage.

Complementary optical identification observations

Also called: Cleavage (mineral)

References & related terms

Tulane University — Physical Properties of Minerals Reference checked 2026-10-24

Additional interpretation reference

Related: Mineral fracture · Conchoidal fracture · Mineral parting · Pleochroism · Optical extinction · Extinction angle · Rock cleavage · Crenulation cleavage · Mineral tenacity

Additional schematic: Flexible versus elastic mineral behaviour

View schematic: Cleavage directions versus fracture

Wellsite geology & samples#

Mineral fracture

Breakage of a mineral along surfaces other than its cleavage planes. Describe the surface character, such as uneven, splintery or conchoidal; a mineral with cleavage may also fracture in other directions.

Mineral identification: cleavage, fracture and parting

Also called: Fracture (mineral)

References & related terms

Tulane University — Physical Properties of Minerals Reference checked 2026-10-24

Related: Conchoidal fracture · Mineral parting

View schematic: Cleavage directions versus fracture

Wellsite geology & samples#

Mineral parting

Planar breakage controlled by particular structural weaknesses, for example those associated with deformation or twinning, rather than the consistently available cleavage planes of the mineral lattice. Parting may occur in some specimens of a mineral and be absent in others.

Mineral identification: cleavage, fracture and parting

Also called: Parting (mineral)

References & related terms

Tulane University — Physical Properties of Minerals Reference checked 2026-10-24

Related: Mineral fracture · Conchoidal fracture

View schematic: Cleavage directions versus fracture

Reservoir engineering#

Miscible fluids

Fluids capable of forming a single homogeneous phase in all proportions under specified pressure and temperature.

References & related terms

SLB Energy Glossary — miscible Reference checked 2026-10-24

Related: Reservoir · Permeability

Petrophysics & log interpretation#

Moldic porosity

Secondary pore space left when a grain or skeletal component dissolves while its original shape remains preserved as a cavity.

Field context Moldic describes pore origin and shape, not connectivity. A dissolved grain can leave an isolated cavity or one linked to other pores. Describe visible moulds separately from measured connected porosity and permeability.

Worked example: visible moulds versus connected porosity

Also called: Mouldic porosity

References & related terms

SLB Energy Glossary — moldic porosity Reference checked 2026-10-29

Field-context reference

Related: Porosity · Resistivity log · Wireline logging · Fossil mould · Fossil cast · Effective porosity · Total porosity · Permeability

View schematic: Porosity and connected flow

Production fluids and facilities#

Mud anchor

Large-diameter intake shroud reducing solids reaching a subsurface rod pump.

References & related terms

SLB Energy Glossary — mud anchor Reference checked 2026-10-24

Related: Gas anchor

Well control#

Mud-gas separator MGS

Surface vessel that separates substantial free gas from returning drilling fluid; it serves a different role from a vacuum degasser.

Also called: Gas buster, Poor boy degasser

References & related terms

SLB — MUD GAS SEPARATOR unit Reference checked 2026-10-24

Related: Degasser · Choke manifold

Reservoir geology#

Mudstone MDST

Fine-grained sedimentary rock composed mainly of mud-sized material; in clastic usage, it lacks the strong fissility of shale.

Field context Here mudstone is used in the clastic sense. Visible lamination can occur without strong fissility; do not confuse a carbonate mudstone classification with this breakage description.

Worked comparison: splitting versus layering

References & related terms

USGS — Lithologic classification of geologic map units Reference checked 2026-10-28

Additional interpretation reference

Related: Bubblepoint pressure · Fault · Fluid saturation · Formation dip · Fissility · Shale · Lamination · Rock cleavage

View schematic: Fissility, lamination and tectonic cleavage

Gas processing and refining#

Natural gas plant liquids NGPL

Hydrocarbons recovered as liquids in gas-processing plants; distinct from lease and plant condensate in EIA reporting.

References & related terms

U.S. EIA Energy Glossary — N Reference checked 2026-10-24

Related: Crude oil · Natural gas liquids

Gas processing and refining#

Natural gasoline

Predominantly pentanes-and-heavier hydrocarbon mixture recovered from natural gas and generally liquid at ambient conditions.

Also called: Pentanes plus

References & related terms

U.S. EIA Energy Glossary — N Reference checked 2026-10-24

Related: Crude oil · Natural gas liquids

Geophysics & seismic#

Normal incidence

A wave approaching an interface along its normal, at zero angle to that normal. For a horizontal interface this path is vertical; normal incidence does not mean zero angle to the interface itself.

Seismic impedance and reflection: worked example

Also called: Perpendicular incidence

References & related terms

University of British Columbia — Normal Incidence Reflection Seismogram Reference checked 2026-10-25

Related: Acoustic impedance · Reflection coefficient · Wavelet

View schematic: Normal-incidence reflection at an impedance contrast

Gas processing and refining#

Olefin

Unsaturated hydrocarbon with a carbon–carbon double bond, commonly produced in refineries and petrochemical plants.

Also called: Alkene, Olefinic hydrocarbon

References & related terms

U.S. EIA Energy Glossary — O Reference checked 2026-10-24

Related: Crude oil · Natural gas liquids

Reservoir geology#

Onlap

Termination of younger, gently inclined beds against an older surface that slopes more steeply.

Field context Read the termination relative to the lower bounding surface and original depositional geometry. In the standard usage, onlap ends updip and downlap ends downdip; present apparent dip alone may be misleading after deformation.

Worked interpretation: reflection terminations and uncertainty

References & related terms

SLB Energy Glossary — onlap Reference checked 2026-10-24

Additional interpretation reference

Related: Downlap · Progradation · Retrogradation · Sequence stratigraphy · Baselap · Toplap

View schematic: Reflection terminations: identify the bounding surface first

Production fluids and facilities#

Orifice meter

Flow-measuring instrument using pressure difference across a known restriction together with fluid and pipe conditions.

References & related terms

SLB Energy Glossary — orifice meter Reference checked 2026-10-24

Related: Multiphase meter

Reservoir geology#

Paleocurrent

A past sediment-transporting current whose direction can be reconstructed from preserved sedimentary evidence, including clast fabrics and cross-stratification.

Field context Keep the measured feature, restored orientation and interpreted flow direction distinct. Local transport evidence does not by itself map a whole drainage basin.

From grain shape to clast fabric

Also called: Palaeocurrent, Ancient current

References & related terms

USGS — Miao et al. (2008), Paleocurrent and fabric analyses Reference checked 2026-10-25

Related: Clast imbrication · Conglomerate · Cross-bedding · Flute cast · Groove cast

View schematic: Clast imbrication and inferred flow

Reservoir geology#

Parasequence

Relatively conformable package of beds bounded by marine flooding surfaces.

Field context Look for genetically related facies between bounding surfaces, not simply a repeating log motif. Shallowing-upward coastal packages are common examples; thickness alone does not define the unit.

Worked example: flooding surfaces and parasequence evidence

References & related terms

SLB Energy Glossary — parasequence Reference checked 2026-10-28

Additional interpretation reference

Related: Lithology · Stratigraphy · Porosity · Marine flooding surface · Maximum flooding surface · Facies

View schematic: Parasequence boundaries and evidence

Reservoir geology#

Parent isotope

A radioactive isotope whose decay is used, with its products and decay rate, in an isotopic dating system.

Field context The measured parent abundance is the amount remaining today; it is not generally the starting amount. A decay model and daughter correction are needed to infer elapsed time.

Radiometric dating: half-life and age interpretation

References & related terms

Minnesota Geological Survey — Geologic Time Reference checked 2026-10-25

Additional interpretation reference

Related: Daughter isotope · Half-life · Radiometric dating · Radiogenic isotope · Closed isotopic system

View schematic: Radioactive decay in a closed teaching system

Reservoir geology#

Permeability K

Measure of how readily a connected pore system transmits fluid under a pressure gradient.

Field context Notation varies between disciplines. Intrinsic permeability is commonly written k and has area units (m² or darcies); hydraulic conductivity is commonly K and has length/time units. Read the stated units and fluid conditions before comparing results.

Worked example: permeability versus hydraulic conductivity

References & related terms

SLB — Reservoir engineering Reference checked 2026-10-24

Field-context reference

Related: Porosity · Water saturation · Fluid saturation · Reservoir · Absolute permeability · Hydraulic conductivity

View schematic: Porosity and connected flow

Reservoir geology#

Phi scale

Logarithmic particle-size coordinate defined by phi = −log2(d / 1 mm), where d is grain diameter. Each increase of one phi unit halves the diameter; positive phi values indicate finer grains than 1 mm.

Field context A mean calculated in phi converts back to a geometric mean diameter, not an arithmetic mean diameter. For equally weighted 0.125 and 0.5 mm observations, mean phi is 2 (0.25 mm); the arithmetic diameter mean is 0.3125 mm. State weighting and statistical method.

Worked example: averaging phi versus diameter

Also called: Krumbein phi scale

References & related terms

IODP Expedition 331 — grain-size comparison Reference checked 2026-10-30

Field-context reference

Related: Grain size · Sorting · Grain roundness

View schematic: Grain size, sorting and grain shape

Petrophysics & log interpretation#

Photoelectric factor log PEF

Log of photoelectric absorption response used to help identify matrix mineralogy, with possible interference from heavy minerals such as barite.

Also called: Photoelectric absorption factor

References & related terms

SLB Energy Glossary — pef Reference checked 2026-10-24

Related: Porosity · Resistivity log · Wireline logging

Production fluids and facilities#

Pig

Device traveling inside a pipeline to clean it, separate batches, displace liquids, or carry inspection equipment.

Also called: Pipeline scraper

References & related terms

SLB Energy Glossary — pig Reference checked 2026-10-24

Related: Pigging · Pig launcher

Production fluids and facilities#

Pigging

Operation of moving a pig through a pipeline for cleaning, fluid displacement, separation, or inspection.

References & related terms

SLB Energy Glossary — pigging Reference checked 2026-10-24

Related: Pig · Pipeline

Reservoir geology#

Pinch-out

Lateral thinning of a rock unit to its termination. A reservoir pinch-out needs an effective seal and other conditions to form a trap.

Also called: Pinchout

References & related terms

SLB Energy Glossary — Pinch-out Reference checked 2026-10-24

Related: Facies · Reservoir

Production fluids and facilities#

Pipeline

Connected piping used to transport petroleum fluids between production, processing, storage, and delivery locations.

References & related terms

SLB Energy Glossary — pipeline Reference checked 2026-10-24

Related: Gathering line · Pigging

Well integrity#

Plug and abandonment P&A

Permanent closure of a well using barriers and other measures required to isolate fluids and leave the well secure.

Also called: plug and abandon, well abandonment

References & related terms

SLB Energy Glossary — Plug and abandonment Reference checked 2026-10-24

Related: Cement plug · Bridge plug

Petrophysics & log interpretation#

Pore throat

Narrow connection between pore bodies that strongly influences fluid flow, electrical conduction and capillary behavior.

Field context For a cylindrical, water-wet throat, entry pressure scales with interfacial tension and the cosine of the contact angle measured through water, and inversely with throat radius. A larger pore body does not remove a narrow connecting throat.

Capillary entry: worked pore-throat example

References & related terms

SLB Energy Glossary — pore throat Reference checked 2026-10-24

Additional interpretation reference

Related: Porosity · Resistivity log · Wireline logging · Capillary pressure · Capillary entry pressure

View schematic: Pore-throat radius and capillary entry

Reservoir geology#

Pore-water pressure

Pressure of water within connected pore spaces. Under hydrostatic conditions it increases with water-column height above the point; groundwater flow can produce a different pressure distribution.

Effective stress and compaction: worked example

Also called: Porewater pressure

References & related terms

UWE GeotechniCAL — Stress in the ground Reference checked 2026-10-25

Related: Effective stress · Total vertical stress · Preconsolidation stress · Compaction

View schematic: Effective stress during pore-pressure decline

Reservoir geology#

Porosity PHI

Fraction of bulk rock volume occupied by pores; it describes storage, not by itself flow capacity.

Field context Use bulk volume, including solids and pores, as the denominator. In a hypothetical 100 cm³ sample with 75 cm³ solids and 25 cm³ pores, porosity is 25%, whereas void ratio is 25/75 = 1/3. Neither ratio measures fluid mobility; state the pore-volume convention and sample condition.

Worked example: total versus effective porosity

References & related terms

SLB — Reservoir engineering Reference checked 2026-10-29

Field-context reference

Related: Permeability · Water saturation · Fluid saturation · Reservoir · Compaction · Core · Void ratio · Volumetric water content

View schematic: Porosity and connected flow

Reservoir geology#

Preconsolidation stress

Effective-stress threshold associated with the loading history and yield of a sediment framework. In aquifer-system models, exceeding it commonly produces substantially greater, largely irreversible compaction than stress changes below it.

Effective stress and compaction: worked example

Also called: Preconsolidation pressure

References & related terms

The Groundwater Project — Effective intergranular stress Reference checked 2026-10-25

Related: Effective stress · Pore-water pressure · Total vertical stress · Compaction

View schematic: Effective stress during pore-pressure decline

Production and artificial lift#

Progressing cavity pump PCP

A rotating helical rotor works inside a stator to move fluid through successive pump cavities.

Also called: progressive cavity pump

References & related terms

SLB Oilfield Review — Artificial Lift Reference checked 2026-10-24

Related: Artificial lift

Reservoir geology#

Radiogenic isotope

An isotope formed by radioactive decay. In geochronology, the radiogenic daughter component must be distinguished from daughter atoms already present when the dated system began retaining them.

Field context A lower retained daughter/parent ratio can reflect daughter loss rather than a younger formation event. The worked loss example holds parent constant; it is not a universal correction for disturbed samples.

Worked example: daughter loss and apparent age

References & related terms

USGS — Radiogenic Isotopes Reference checked 2026-10-29

Field-context reference

Additional interpretation reference

Related: Radiometric dating · Parent isotope · Daughter isotope · Half-life · Closed isotopic system · Isotope delta · Isotope fractionation

View schematic: Radioactive decay in a closed teaching system

Reservoir geology#

Radiometric dating

Estimating geological ages from radioactive parent isotopes, their decay products and known decay behaviour.

Field context An age refers to the event recorded by the selected mineral and isotope system, potentially crystallization, cooling or later disturbance. A detrital grain age does not directly date sediment deposition. In a closed single-step model with a fixed 10-million-year half-life, radiogenic daughter/parent ratios of 6.6, 7.0 and 7.4 give elapsed times of 29.260, 30.000 and 30.704 million years. Symmetric ratio bounds need not give symmetric age bounds; these stipulated limits are not a laboratory confidence interval. Pooling parent and daughter amounts from components of different ages can yield an apparent age that is neither their arithmetic mean nor evidence of a distinct geological event.

Worked example: pooled amounts versus mean ages

Also called: Isotopic dating

References & related terms

Minnesota Geological Survey — Geologic Time Reference checked 2026-10-30

Field-context reference

Additional interpretation reference

Related: Parent isotope · Daughter isotope · Half-life · Relative dating (Geology Dictionary) · Superposition (Geology Dictionary) · Cross-cutting relationship (Geology Dictionary) · Radiogenic isotope · Closed isotopic system · Thermochronology · Closure temperature · Polarity zone · Polarity chron · Detrital zircon · Maximum depositional age

Additional schematic: Pooling isotope amounts versus averaging ages

View schematic: Radioactive decay in a closed teaching system

Drilling operations#

Reaming

Working through an existing hole with cutting or sizing equipment to restore clearance or enlarge its diameter.

Also called: Ream

References & related terms

SLB Energy Glossary — Reaming Reference checked 2026-10-24

Related: Wiper trip

Geophysics & seismic#

Reflection coefficient

Ratio of reflected to incident wave amplitude at an interface, dependent on the properties on either side.

Field context For normal-incidence pressure amplitudes from layer 1 to layer 2, R = (Z2 − Z1)/(Z2 + Z1). A positive value indicates increasing impedance. R is an amplitude ratio, not a reflected-energy fraction; in the ideal lossless case that fraction is R². In the same lossless normal-incidence pressure convention, transmitted amplitude ratio is 1 + R; transmitted energy fraction also requires the incident-to-transmitted impedance ratio.

Worked example: transmitted amplitude and energy balance

References & related terms

SLB Energy Glossary — reflection coefficient Reference checked 2026-10-24

Field-context reference

Additional interpretation reference

Related: Acoustic impedance · Synthetic seismogram · Sonic log · Normal incidence · Reflectivity series

Additional schematic: Normal-incidence reflection at an impedance contrast

View schematic: Acoustic impedance and seismic reflection

Geophysics & seismic#

Reflectivity series

A sequence of interface reflection coefficients located at their travel times in a layered seismic model. Convolving this sequence with a chosen wavelet produces a simplified synthetic trace; the coefficients alone are not the recorded waveform.

Field context A coefficient at a deeper interface is not automatically the returned primary amplitude: transmission through overlying boundaries modifies the wave on both its downward and upward paths. State whether the synthetic includes these factors, multiples and propagation losses.

Worked example: two transmissions and one deeper reflection

Also called: Reflectivity function

References & related terms

University of British Columbia — Normal Incidence Reflection Seismogram Reference checked 2026-10-25

Related: Acoustic impedance · Reflection coefficient · Wavelet

View schematic: Normal-incidence reflection at an impedance contrast

Production fluids and facilities#

Retention time

Average duration liquid remains in a vessel, commonly estimated as liquid inventory divided by volumetric throughput.

Also called: Residence time

References & related terms

SLB Energy Glossary — retention time Reference checked 2026-10-24

Related: Test separator · Coalescence

Reservoir geology#

Reworked fossil

A fossil eroded from an earlier deposit and incorporated into later sediment. Its original age can be older than the bed that now contains it.

Field context Reworking is a depositional history; drilling cavings are sample contamination. Do not interpret a mixed fossil assemblage until these possibilities have been considered. Fossils introduced through burrows or other pathways are a separate possibility; mixed ages alone do not demonstrate erosion and redeposition.

Worked example: reworking versus drilling cavings

Also called: Redeposited fossil

References & related terms

National Park Service — Fossils in Parks Reference checked 2026-10-29

Field-context reference

Additional interpretation reference

Related: Fossil · Biostratigraphy · Taxon-range zone · Concurrent-range zone · Cavings

Additional schematic: Fossil reworking and drilling cavings

View schematic: Fossil reworking: two burial histories

Geosteering & modelling#

Right-hand rule RHR

Convention for recording a plane by choosing the strike bearing that puts its down-dip side to the observer’s right. In the Canadian convention used here, dip azimuth equals strike azimuth plus 90°, reduced modulo 360°.

Worked example: strike and apparent dip

Also called: Right dip rule

References & related terms

Géologie Québec — Structural measurements on outcrops Reference checked 2026-10-25

Related: Strike · Formation dip · Apparent dip · Dip direction

View schematic: Strike, dip direction and apparent dip

Drilling dynamics & BHA#

Rotary steerable system RSS

Downhole steering equipment that controls direction while the drillstring rotates.

Field context Continuous surface rotation does not mean every RSS uses the same steering mechanism. Push-the-bit and point-the-bit systems apply directional control in different ways.

References & related terms

SLB — Directional drilling practices Reference checked 2026-10-24

Field-context reference

Related: Directional drilling · Geosteering · Kickoff point · Build section · Mud motor

View schematic: Well geometry: along-hole and vertical depth

Production and reservoir performance#

Scale

Mineral deposits formed when dissolved constituents precipitate from fluids, potentially restricting equipment or reservoir flow paths.

Also called: mineral scale

References & related terms

SLB Oilfield Review — Formation Damage Reference checked 2026-10-24

Related: Formation damage

Geophysics & seismic#

Seismic datum

Reference surface to which seismic observations are corrected to reduce effects of elevation and near-surface conditions.

Field context Depth and time must refer to consistent reference surfaces. State the seismic reference datum and the well depth origin before comparison; metres below datum, elevation and measured depth along a deviated borehole are not interchangeable.

Worked example: two layers, travel time and depth

References & related terms

SLB Energy Glossary — datum Reference checked 2026-10-24

Field-context reference

Related: Acoustic impedance · Synthetic seismogram · Sonic log · Average seismic velocity · Depth conversion

View schematic: Two layers: travel time and depth are different coordinates

Geophysics & seismic#

Seismic tuning

Interference between reflections from closely spaced boundaries that changes the apparent amplitude and shape of a thin-bed response.

Field context Compare a calculated summed wavelet response with interface times before equating trace extrema with bed boundaries. Sample spacing alone does not establish boundary separability.

Worked example: two interfaces and a summed seismic trace

Also called: Tuning effect

References & related terms

SLB Energy Glossary — tuning effect Reference checked 2026-10-29

Field-context reference

Related: Acoustic impedance · Synthetic seismogram · Sonic log · Seismic wavelength · Vertical seismic resolution

View schematic: Wavelength and a quarter-wavelength separability estimate

Reservoir geology#

Shale SH

Fine-grained sedimentary rock that commonly splits along closely spaced layers; clay minerals and silt are typical constituents.

Field context Record fissility independently of colour and lamination. Plate-like cuttings alone do not identify a cleavage origin, clay species or geographic orientation.

Worked comparison: splitting versus layering

References & related terms

USGS — Lithologic classification of geologic map units Reference checked 2026-10-28

Additional interpretation reference

Related: Bubblepoint pressure · Fault · Fluid saturation · Formation dip · Fissility · Mudstone · Lamination · Rock cleavage

View schematic: Fissility, lamination and tectonic cleavage

Cementing and casing#

Shoe track

The casing section below the float collar that retains cement as a placement margin near the shoe.

Also called: float joint

References & related terms

SLB Energy Glossary — Shoe track Reference checked 2026-10-24

Related: Cementing · Casing

Well intervention#

Sinker bar

Weight section in a slickline tool string that helps it descend and supplies mass for tool operation.

Also called: slickline stem

References & related terms

SLB Energy Glossary — Sinker bar Reference checked 2026-10-24

Related: Slickline · Jar

Well intervention#

Snubbing

Inserting tubulars into a pressurized well when pressure-generated upward force requires controlled mechanical restraint.

References & related terms

SLB Energy Glossary — Snubbing Reference checked 2026-10-24

Related: Well intervention

Wellsite geology & samples#

Solvent cut

Observation of material dissolving or diffusing into solvent during sample-show assessment; interpreted together with fluorescence and contamination checks.

Also called: Cut test

References & related terms

SLB — Defining Mud Logging Reference checked 2026-10-24

Related: Mud logging · Gas show · Cuttings

Reservoir geology#

Sorting

Spread of grain sizes within sediment: a narrow spread is well sorted, while a broad mixture is poorly sorted.

Field context Sorting describes the spread of sizes, not whether the average grain is fine or coarse. A visual estimate should not be reported as a calculated standard deviation; state the statistical method and weighting when measured. Number-weighted image counts and mass-weighted sieve fractions are not interchangeable; record the weighting and any excluded fines.

Worked example: grain counts versus mass fractions

References & related terms

SLB Energy Glossary — Sorting Reference checked 2026-10-29

Additional interpretation reference

Related: Grain size · Grain roundness · Phi scale · Grain sphericity · Median grain size · Sieve analysis

View schematic: Grain size, sorting and grain shape

Petroleum fluids and properties#

Specific gravity

Dimensionless density ratio to a stated reference material; liquid petroleum measurements commonly use water.

Field context For mineral comparison, state the water reference and conditions. Specific gravity has no units; it is not the same numerical value as density expressed in kg/m³. For an ideal impermeable specimen, hydrostatic weighing uses air weight divided by apparent weight loss in water, not by the submerged reading itself. Readings of 2.65 N and 1.65 N give 2.65/(2.65 − 1.65) = 2.65.

Worked example: apparent weight loss in water

Also called: s.g.

References & related terms

SLB Energy Glossary — specific gravity Reference checked 2026-10-30

Field-context reference

Additional interpretation reference

Related: Density · API gravity

View schematic: Density and specific gravity: equal-volume comparison

Hydrogeology & pore systems#

Specific storage

Water volume released from saturated storage per unit bulk aquifer volume per unit decrease in hydraulic head, for specified mechanical conditions. Specific storage has inverse-length units and accounts for changes in pore volume and water density.

Field context For fully saturated layers sharing the same head decline, sum Ss × layer thickness to obtain column storativity; the equivalent Ss is thickness-weighted. If declines differ by layer, calculate each storage-volume change separately. This accounting does not determine the transient heads or a sustainable pumping rate.

Worked example: thickness-weighted confined storage

References & related terms

The Groundwater Project — aquifer transmission and storage Reference checked 2026-10-31

Related: Storativity · Transmissivity

View schematic: Thickness weighting in confined storage

MWD, LWD & telemetry#

Spectral gamma ray SGR

Natural gamma-ray measurement separated by energy to estimate contributions from potassium, uranium and thorium. It adds compositional information beyond a single total gamma-ray curve.

Field context Keep total GR (API or stated count units) separate from calibrated K (weight %), U and Th (ppm). Do not add elemental concentrations directly to obtain total GR; confirm the curve definition and calibration.

Worked interpretation: equal total GR, different evidence

References & related terms

Halliburton — spectral gamma ray Reference checked 2026-10-29

Additional interpretation reference

Related: Logging while drilling · Measurement while drilling · Distance to bit · Total gamma ray · Gamma ray log

View schematic: Total GR and spectral components

Drilling dynamics & BHA#

Stick-slip

Torsional motion in which the bit or drillstring alternately slows or stops and then accelerates as stored twist is released.

Also called: Stick/slip

References & related terms

SLB Energy Glossary — Stick-slip Reference checked 2026-10-24

Related: Torque · Rotary speed

Hydrogeology & pore systems#

Storativity

Water volume released from storage per unit aquifer plan area per unit decline in hydraulic head. It is dimensionless. In a uniform confined aquifer S = Ss b; unconfined storage also includes gravity drainage.

Field context For spatially variable head decline, sum S × area × local decline across representative zones. With constant S, use the area-weighted mean decline, not the maximum observed decline; pumped volume can also include boundary inflow.

Worked example: spatial drawdown and storage release

Also called: Storage coefficient

References & related terms

The Groundwater Project — aquifer transmission and storage Reference checked 2026-10-25

Related: Specific storage · Transmissivity · Hydraulic diffusivity

View schematic: Confined aquifer: head decline and stored water

Depth & surveys#

Strike

Horizontal direction of a line on a geological plane, normally stated relative to a north reference.

Field context Strike alone has two opposite bearings. Record the dip side or state the orientation convention; a horizontal plane has no unique strike.

Worked example: strike and apparent dip

References & related terms

SLB Energy Glossary — Strike Reference checked 2026-10-25

Additional interpretation reference

Related: Formation dip · Apparent dip · Dip direction · Right-hand rule

View schematic: Strike, dip direction and apparent dip

Production chemistry#

Surfactant

Surface-active chemical that changes interfacial behavior, including wetting, emulsification, or foaming.

References & related terms

SLB Energy Glossary — surfactant Reference checked 2026-10-24

Related: Emulsion · Scale

Reservoir engineering#

Sweep efficiency

Fraction of the relevant reservoir volume contacted by an injected displacement fluid.

Also called: volumetric sweep efficiency, volumetric displacement efficiency

References & related terms

SLB Energy Glossary — sweep efficiency Reference checked 2026-10-24

Related: Reservoir · Permeability

Reservoir geology#

Syncline

Fold containing younger beds in its core, commonly forming a trough.

Field context Separate fold shape from stratigraphic age: antiform and synform describe closure, whereas anticline and syncline require age evidence. Record the profile orientation before measuring limb angles.

Worked example: fold profile and bed age

References & related terms

SLB Energy Glossary — syncline Reference checked 2026-10-24

Additional interpretation reference

Related: Anticline · Fold · Structural trap · Synform · Interlimb angle · Antiform

View schematic: Fold profile: shape, limb angle and bed age

Cementing and casing#

Thickening time

The laboratory-measured interval during which cement slurry remains pumpable under a specified temperature and pressure schedule.

References & related terms

SLB Energy Glossary — Thickening time Reference checked 2026-10-24

Related: Cementing · Casing

Geosteering & modelling#

Three-dimensional formation model 3D model

Model allowing geological properties and boundaries to vary in all three spatial directions. Greater geometric flexibility requires more input information and does not guarantee a unique interpretation.

References & related terms

SLB Energy Glossary — forward modeling Reference checked 2026-10-24

Related: Geosteering · Forward modelling · Log correlation

Geosteering & modelling#

Three-dimensional resistivity inversion 3D inversion

Estimation of a spatial resistivity model from measured electromagnetic responses while allowing variation in three dimensions. The resulting image remains model-dependent and may have nonunique solutions.

References & related terms

Halliburton — 3D ultra-deep resistivity Reference checked 2026-10-24

Related: Geosteering · Forward modelling · Log correlation

Rig equipment#

Top drive

Travelling drive system suspended in the derrick that rotates the drillstring and provides a drilling-fluid connection.

References & related terms

SLB Energy Glossary — Top drive Reference checked 2026-10-24

Related: Kelly · Rotary table

MWD, LWD & telemetry#

Total gamma ray

Combined natural gamma-ray response rather than separate spectral components. Similar total readings can arise from different mineral or radioactive-element combinations.

Field context Keep total GR (API or stated count units) separate from calibrated K (weight %), U and Th (ppm). Do not add elemental concentrations directly to obtain total GR; confirm the curve definition and calibration.

Worked interpretation: equal total GR, different evidence

References & related terms

Halliburton — spectral gamma ray Reference checked 2026-10-29

Additional interpretation reference

Related: Logging while drilling · Measurement while drilling · Distance to bit · Spectral gamma ray · Gamma ray log

View schematic: Total GR and spectral components

Petrophysics & log interpretation#

Total porosity

Fraction of bulk rock volume occupied by all pores, including isolated pores and pore space associated with clay-bound water.

Field context Keep the bulk-volume denominator and measurement method explicit. Total pore volume includes isolated space; it does not establish connected flow, permeability or producible fluid volume. Combine disjoint rock volumes by adding their pore volumes and dividing by their summed bulk volume. A simple mean of porosity percentages is valid only for equal represented bulk volumes on a consistent measurement basis.

Worked example: volume-weighted porosity

References & related terms

SLB Energy Glossary — total porosity Reference checked 2026-10-29

Field-context reference

Related: Effective porosity · Primary porosity · Secondary porosity · Porosity

Additional schematic: Porosity: add volumes before dividing

View schematic: Porosity and connected flow

Reservoir geology#

Total vertical stress

Vertical force per unit horizontal area carried by the combined solid-fluid system, arising from the weight of overlying material and surface loads. It differs from the effective stress carried by the framework.

Effective stress and compaction: worked example

Also called: Vertical overburden stress

References & related terms

UWE GeotechniCAL — Stress in the ground Reference checked 2026-10-25

Related: Effective stress · Pore-water pressure · Preconsolidation stress · Compaction

View schematic: Effective stress during pore-pressure decline

Reservoir geology#

Trace fossil

Preserved evidence of organism activity, such as a burrow or track, rather than the organism’s body.

Field context A trace records activity. Describe its host surface and preservation context separately from associated body fossils.

Fossil preservation and reworking: worked interpretation

References & related terms

Texas A&M Ocean Drilling Program — Sedimentary rock classification Reference checked 2026-10-24

Field-context reference

Related: Facies · Depositional environment · Reworked fossil · Fossil disarticulation · Firmground · Hardground · Ichnofabric · Ichnofacies

View schematic: Firm and lithified substrates at colonization

Hydrogeology & pore systems#

Transmissivity

Hydraulic conductivity integrated through saturated aquifer thickness. For uniform conductivity K and thickness b, T = Kb, with area-per-time units; it describes transmission capacity rather than stored water volume.

Field context T has area-per-time units. A head decline above a confined aquifer roof need not reduce saturated thickness; a declining unconfined water table generally does.

Aquifer transmission and storage example

References & related terms

The Groundwater Project — aquifer transmission and storage Reference checked 2026-10-25

Related: Specific storage · Storativity · Hydraulic diffusivity

View schematic: Confined aquifer: head decline and stored water

Well control#

Trip tank

Small calibrated vessel used to monitor fluid-volume changes associated with moving tubulars into or out of a well.

References & related terms

IWCF — Trip tank Reference checked 2026-10-24

Related: Tripping · Swabbing while tripping

Geosteering & modelling#

True stratigraphic thickness TST

Thickness measured perpendicular to bedding. In a well it requires accounting for bed orientation and borehole trajectory.

Field context For parallel planar contacts, TST = TVT × cos(true dip). A hypothetical 10.00 m vertical interval at 30° dip represents 8.66 m normal thickness. Along-hole length is a different measurement: its correction depends on the angle between the local trajectory and the bedding normal. Fault repetition or changing bed orientation invalidates a single-plane correction.

Worked example: vertical, normal and along-hole thickness

References & related terms

SLB Energy Glossary — True stratigraphic thickness Reference checked 2026-10-28

Additional interpretation reference

Related: True vertical thickness · Isopach · Formation dip

View schematic: Bedding dip and thickness

Geosteering & modelling#

True vertical thickness TVT

Vertical separation between the top and base of a unit at the same horizontal location; distinct from along-hole thickness.

Field context For parallel planar contacts, TST = TVT × cos(true dip). A hypothetical 10.00 m vertical interval at 30° dip represents 8.66 m normal thickness. Along-hole length is a different measurement: its correction depends on the angle between the local trajectory and the bedding normal. Fault repetition or changing bed orientation invalidates a single-plane correction.

Worked example: vertical, normal and along-hole thickness

References & related terms

SLB Energy Glossary — True vertical thickness Reference checked 2026-10-28

Additional interpretation reference

Related: True stratigraphic thickness · Isochore

View schematic: Bedding dip and thickness

Reservoir geology#

Turbidite

Sediment deposited by a turbidity current, often showing upward grading from coarser to finer material.

Field context Describe grading within individual beds separately from a grain-size trend through several beds. A normally graded bed alone does not prove a turbidity-current origin; evaluate the complete sedimentary context. Sole markings may record erosion by a different flow from the one that deposited the overlying sand.

Worked example: grading within one bed

References & related terms

SLB Energy Glossary — turbidite Reference checked 2026-10-24

Field-context reference

Additional interpretation reference

Related: Lithology · Stratigraphy · Porosity · Flute cast · Groove cast

View schematic: Flute casts and groove casts: direction versus axis

Geophysics & seismic#

Two-way travel time TWT

Elapsed time for seismic energy to travel from a source to a reflector and back to a receiver.

Field context Keep seconds and milliseconds explicit. For the ideal vertical path to a horizontal reflector, depth below a common datum is average velocity multiplied by half the two-way time. A recorded nonzero-offset arrival or a dipping reflector requires the appropriate imaging and ray-path treatment.

Worked example: two layers, travel time and depth

Also called: Two-way traveltime

References & related terms

SLB Energy Glossary — two-way traveltime Reference checked 2026-10-24

Field-context reference

Related: Acoustic impedance · Synthetic seismogram · Sonic log · Average seismic velocity · Depth conversion

View schematic: Two layers: travel time and depth are different coordinates

Geosteering & modelling#

Ultra-deep resistivity UDR

Resistivity measurement designed to investigate farther from the borehole than conventional shallow measurements. Useful detection distance depends on geology, resistivity contrast, tool configuration and interpretation.

References & related terms

Halliburton — 3D ultra-deep resistivity Reference checked 2026-10-24

Related: Geosteering · Forward modelling · Log correlation

Reservoir geology#

Unconformity

Surface representing a gap in the preserved geological record caused by erosion, nondeposition or both.

Field context Record the evidence for a break and assess its significance before selecting it as a unit boundary.

Worked example: choose the bounding breaks

References & related terms

SLB Energy Glossary — Unconformity Reference checked 2026-10-24

Additional interpretation reference

Related: Stratigraphy · Formation · Diastem · Hiatus · Synthem

View schematic: Synthem boundaries and an internal depositional pause

Production and artificial lift#

Variable-speed drive VSD

Electrical equipment that adjusts motor operating speed, allowing a lift system to respond to changing well conditions.

Also called: variable frequency drive, VFD

References & related terms

SLB Oilfield Review — Artificial Lift Reference checked 2026-10-24

Related: Electric submersible pump

Drilling problems#

Washout

Eroded enlargement of an open hole; the same term can describe an erosion leak through a tubular or connection. Specify the context.

References & related terms

SLB Energy Glossary — Washout Reference checked 2026-10-24

Related: Drill pipe · Casing

Reservoir engineering#

Water drive

Natural reservoir support from water moving out of a connected aquifer as hydrocarbons are withdrawn.

Also called: waterdrive

References & related terms

SLB Energy Glossary — waterdrive Reference checked 2026-10-24

Related: Reservoir · Permeability

Drilling fluids#

Water-based mud WBM

Drilling fluid whose continuous liquid phase is water, with solids and additives selected for the well conditions.

Also called: Water-based drilling fluid

References & related terms

IADC Lexicon — Water-based mud Reference checked 2026-10-24

Related: Oil-based mud · Drilling mud

Geophysics & seismic#

Wavelet

Short seismic pulse characterized by its amplitude, phase and frequency content.

Field context A simplified synthetic trace adds time-shifted copies of the selected wavelet scaled by interface coefficients. Nearby events can overlap. Confirm wavelet phase and display polarity before interpreting a peak or trough as an impedance increase.

Seismic impedance and reflection: worked example

References & related terms

SLB Energy Glossary — wavelet Reference checked 2026-10-24

Field-context reference

Related: Acoustic impedance · Synthetic seismogram · Sonic log · Normal incidence · Reflectivity series · Seismic wavelength · Vertical seismic resolution

View schematic: Normal-incidence reflection at an impedance contrast

Petroleum fluids and properties#

Wet gas

Natural gas containing appreciable heavier hydrocarbons; in dehydration work, the phrase may instead mean water-bearing gas.

References & related terms

SLB Energy Glossary — wet gas Reference checked 2026-10-24

Related: Dry natural gas · Dehydrator

Reservoir engineering#

Wettability

Preference of a solid surface for contact with one fluid rather than another.

Field context For a cylindrical, water-wet throat, entry pressure scales with interfacial tension and the cosine of the contact angle measured through water, and inversely with throat radius. A larger pore body does not remove a narrow connecting throat.

Capillary entry: worked pore-throat example

References & related terms

SLB Energy Glossary — wettability Reference checked 2026-10-24

Additional interpretation reference

Related: Contact angle · Imbibition · Drainage displacement · Capillary pressure · Capillary entry pressure · Capillary-pressure hysteresis

View schematic: Pore-throat radius and capillary entry

Drilling operations#

Wiper trip

Partial or complete movement of the drillstring through an existing interval to assess or improve hole condition before further work.

References & related terms

SLB Energy Glossary — Wiper trip Reference checked 2026-10-24

Related: Tripping · Reaming

Health, safety and environment#

Workplace Hazardous Materials Information System WHMIS

Canadian workplace chemical-hazard communication system using classification, labels, safety data sheets, and training.

References & related terms

CCOHS — WHMIS Safety Data Sheet Reference checked 2026-10-24

Related: Hazard class · Hazard statement

Hydrogeology & pore systems#

Specific yield

Volume of water a saturated material releases by gravity drainage divided by its bulk volume. It is dimensionless, not a pumping rate. Drainage is not instantaneous; measurement duration and water-table position affect the result.

Field context Normalize the collected drainage volume by the whole sample volume, not just its initial pore-water volume. In the guide example, 0.18 m³ collected from 1.00 m³ of material gives Sy = 0.18, although 60% of the initial water drains. A finite-duration drainage test gives a time-specific result: in a fixed 1 m³ sample initially holding 0.30 m³ water, cumulative drainage of 0.10 m³ at 1 hour and 0.18 m³ at 24 hours gives measured yield ratios 0.10 and 0.18. The second result does not establish ultimate yield; record duration and drainage boundary conditions.

Worked example: specific yield and retained water

References & related terms

USGS Groundwater Resources Program — Estimating specific yield Reference checked 2026-10-31

Additional interpretation reference

Related: Porosity · Specific storage · Storativity · Specific retention

View schematic: Gravity drainage: account for all the water

Hydrogeology & pore systems#

Specific retention

Volume of water retained against gravity drainage divided by the bulk volume of the porous material. Under the corresponding drainage convention, porosity equals specific yield plus specific retention. Retention depends on drainage conditions and time.

Field context Water remaining at a stated drainage endpoint is still part of the pore volume. In the guide example, 0.12 m³ retained in 1.00 m³ of material gives Sr = 0.12. Record test duration and conditions before comparing results.

Worked example: specific yield and retained water

References & related terms

USGS Groundwater Resources Program — Estimating specific yield Reference checked 2026-10-25

Additional interpretation reference

Related: Porosity · Specific storage · Storativity · Specific yield

View schematic: Gravity drainage: account for all the water

Reservoir geology#

Capillary fringe

Water-saturated or nearly saturated interval immediately above a water table, supported by capillary forces at pore-water pressures below atmospheric pressure.

Field context Its upper boundary is not the water table. Pore-size variation produces a transition rather than a universal fixed thickness; specify whether a description uses full saturation or includes the near-saturated transition.

Worked example: saturation and water pressure

Also called: Capillary zone

References & related terms

Penn State EARTH 111 — Aquifer Anatomy Reference checked 2026-10-25

Related: Water table · Vadose zone · Capillary pressure · Pore-water pressure

View schematic: Capillary fringe: saturation is not pressure

Reservoir geology#

Vadose zone

Subsurface interval above the water table, commonly containing both air and water in its pore space. In the pressure-based usage adopted here it includes the capillary fringe.

Field context Unsaturated zone is a common broad synonym, but a strictly saturation-based boundary lies above the saturated part of the capillary fringe. State the convention when describing a moisture profile.

Worked example: saturation and water pressure

Also called: Zone of aeration, Unsaturated zone

References & related terms

The Groundwater Project — Distribution of Water in the Shallow Subsurface Reference checked 2026-10-25

Related: Water table · Capillary fringe · Pore-water pressure

View schematic: Capillary fringe: saturation is not pressure

Reservoir geology#

Water table

Surface in an unconfined groundwater system where pore-water pressure equals atmospheric pressure: gauge pressure is zero.

Field context Capillary water can saturate pores above this surface. A stabilized shallow well connected to the unconfined unit helps locate it; a confined piezometric level is a different quantity.

Worked example: saturation and water pressure

References & related terms

Penn State EARTH 111 — Aquifer Anatomy Reference checked 2026-10-25

Additional interpretation reference

Related: Capillary fringe · Vadose zone · Pore-water pressure · Gaining stream · Losing stream

View schematic: Capillary fringe: saturation is not pressure

Reservoir geology#

Chronostratigraphic unit

A tangible body of rock representing a specified interval of geological time; formal ranks include eonothem, erathem, system, series and stage.

Field context Use the rock term for the mapped or correlated succession and the paired geochronologic term for the interval of time. For example, Jurassic System refers to rocks; Jurassic Period refers to time. The five illustrated pairs are principal ranks; subsidiary ranks also exist. Boundary definitions may use a GSSP or a GSSA; a GSSP numerical calibration is distinct from its defining point.

Guide: rocks versus geological time

Also called: Time-rock unit

References & related terms

International Commission on Stratigraphy — Chronostratigraphic Units Reference checked 2026-10-25

Related: Geochronologic unit · Hiatus · Radiometric dating · Global Boundary Stratotype Section and Point · Global Standard Stratigraphic Age

View schematic: Chronostratigraphic rocks and geochronologic time

Reservoir geology#

Geochronologic unit

An interval of geological time corresponding to the interval during which a chronostratigraphic unit formed; formal ranks include eon, era, period, epoch and age.

Field context A geochronologic unit is time, not a thickness of rock. Local erosion or nondeposition can remove part of the corresponding rock record without removing that interval from the time scale. The five illustrated pairs are principal ranks; subsidiary ranks also exist. Boundary definitions may use a GSSP or a GSSA; a GSSP numerical calibration is distinct from its defining point.

Guide: rocks versus geological time

Also called: Geologic-time unit

References & related terms

International Commission on Stratigraphy — Chronostratigraphic Units Reference checked 2026-10-25

Related: Chronostratigraphic unit · Hiatus · Radiometric dating · Global Boundary Stratotype Section and Point · Global Standard Stratigraphic Age

View schematic: Chronostratigraphic rocks and geochronologic time

Reservoir geology#

Isochronous

Representing the same geological time at different locations. An isochronous horizon is a time surface, regardless of changes in rock type along it.

Worked example: rock boundary versus time surface

Also called: Synchronous (stratigraphy)

References & related terms

International Commission on Stratigraphy — Chronostratigraphic Units Reference checked 2026-10-25

Related: Diachronous · Chronostratigraphic unit · Formation

View schematic: A rock boundary can cross time surfaces

Reservoir geology#

Hiatus

A span of geological time missing from a local stratigraphic succession because sediment was not deposited, material was eroded, or both. Its duration requires independent evidence.

Field context A preserved-thickness/time average spanning a hiatus includes the gap in its denominator. Recovering a rate for depositional intervals alone requires independent constraints on their duration and on erosion and compaction.

Worked example: hiatus and accumulation-rate denominators

Also called: Stratigraphic gap

References & related terms

ICS Stratigraphic Guide — Unconformity-bounded Units Reference checked 2026-10-25

Field-context reference

Related: Unconformity · Diastem · Synthem · Barren interval

Additional schematic: Hiatus and average accumulation rate

View schematic: Synthem boundaries and an internal depositional pause

Reservoir geology#

Interlimb angle

The angle between the limbs of a fold measured in its profile plane, commonly using tangents to the folded surface at adjacent inflection points. It describes fold tightness; state the classification scheme when assigning a descriptive class.

Field context An oblique section can make a fold appear more open. In the guide’s horizontal-axis example, a section 45° to strike gives apparent limb dips of 22.2° and 40.1°: their 117.7° section angle is not the true 100° interlimb angle. Measure in the profile plane perpendicular to the hinge.

Worked example: fold profile and bed age

Also called: Inter-limb angle

References & related terms

Waldron and Snyder — Introduction to Folds, Lab 4 Reference checked 2026-10-30

Field-context reference

Related: Fold · Anticline · Syncline · Synform · Antiform

View schematic: Fold profile: shape, limb angle and bed age

Reservoir geology#

Younging direction

The direction through a stratified succession toward younger beds, inferred from age relations or reliable primary structures. It describes stratigraphic order and may point downward in the present-day reference frame.

Field context Use several consistent indicators where possible. Grain-size grading must first be identified as normal rather than inverse; an isolated grain-size trend is not conclusive. Cross-bed truncation can provide another test when the depositional boundary and sample orientation are preserved.

Worked example: which way is stratigraphic up?

Also called: Stratigraphic way-up

References & related terms

Waldron and Snyder — Primary Structures Reference checked 2026-10-28

Additional interpretation reference

Related: Normal grading · Fold · Overturned bedding · Cross-bedding

Additional schematic: Cross-bed truncation and stratigraphic way-up

View schematic: Present vertical and stratigraphic younging

Reservoir geology#

Overturned bedding

Bedding whose original stratigraphic top has been rotated past vertical so that its younging direction has a downward component. Establish the original top independently of the present dip.

Field context An overturned limb does not establish the facing of the whole fold. Fold facing is younging within the axial surface, perpendicular to the hinge; it requires additional structural context.

Worked example: which way is stratigraphic up?

Also called: Overturned strata

References & related terms

Earle — Physical Geology 2e: Folding Reference checked 2026-10-25

Related: Normal grading · Fold · Younging direction

View schematic: Present vertical and stratigraphic younging

Reservoir geology#

Lineation

A geological fabric or structure defined by the preferred alignment of linear elements, such as elongate minerals, stretched objects, fold hinges or the intersection of two planar fabrics.

Field context Name the fabric element and record trend and plunge. Different lineations in the same rock may record different structures or deformation stages; do not assign a fold axis or movement direction from the word lineation alone.

Worked example: separate lineation mechanisms

Also called: Linear fabric

References & related terms

Waldron and Snyder — Geological Structures: Fabrics Reference checked 2026-10-26

Related: Intersection lineation · Crenulation lineation · Stretching lineation · Fold · Trend · Plunge · Rake

View schematic: Lineation mechanisms and interpretation checks

Reservoir geology#

Intersection lineation

The line formed where two nonparallel planar fabrics intersect, such as bedding cut by cleavage.

Field context Identify both planes. Bedding–axial-planar-cleavage intersection may approximate a cylindrical fold axis, but that interpretation requires the cleavage relationship and fold geometry to be established.

Worked example: separate lineation mechanisms

Also called: Planar-fabric intersection lineation

References & related terms

Waldron and Snyder — Geological Structures: Fabrics Reference checked 2026-10-26

Related: Lineation · Crenulation lineation · Stretching lineation · Fold

View schematic: Lineation mechanisms and interpretation checks

Reservoir geology#

Crenulation lineation

A linear fabric defined by the aligned hinges of closely spaced small folds that deform an earlier foliation.

Field context It is commonly a second or later fabric. Record which earlier foliation is crenulated and distinguish hinge lines from the axial surfaces that may define crenulation cleavage.

Worked example: separate lineation mechanisms

Also called: Crenulation hinge lineation

References & related terms

Waldron and Snyder — Geological Structures: Fabrics Reference checked 2026-10-26

Related: Lineation · Intersection lineation · Stretching lineation · Fold · Rock cleavage · Crenulation cleavage

View schematic: Lineation mechanisms and interpretation checks

Reservoir geology#

Stretching lineation

A lineation defined by elongate minerals, clasts or other objects stretched and aligned during deformation, commonly parallel to the direction of maximum finite extension recorded by that fabric.

Field context Finite extension is not automatically the same as slip direction, transport direction or fold-axis trend. Establish kinematic context independently before making a movement interpretation.

Worked example: separate lineation mechanisms

Also called: Extension lineation

References & related terms

Waldron and Snyder — Geological Structures: Fabrics Reference checked 2026-10-26

Related: Lineation · Intersection lineation · Crenulation lineation · Fold · Finite strain · Strain ellipse

View schematic: Lineation mechanisms and interpretation checks

Reservoir geology#

Trend

The azimuth of the horizontal projection of a geological line, conventionally recorded toward its downward-plunging end. State the north reference and pair the trend with the plunge.

Field context For an unoriented horizontal line the two opposite bearings describe the same axis; for a vertical line the horizontal projection vanishes and trend is undefined.

Worked example: trend, plunge and rake

Also called: Lineation trend

References & related terms

Géologie Québec — Structural Measurements Reference checked 2026-10-26

Related: Rake · Plunge · Lineation

View schematic: Trend and plunge: two views of one line

Reservoir geology#

Rake

The angle measured within a specified plane between a line lying in that plane and a stated strike direction. Also called pitch; reconstructing the line in geographic coordinates requires the attitude of the host plane and the measurement convention.

Field context An acute pitch needs the referenced strike end and direction toward the line. Signed fault-slip rake uses another convention; retain that convention explicitly. Rake is generally different from plunge.

Worked example: trend, plunge and rake

Also called: Pitch of a lineation, Structural pitch

References & related terms

Géologie Québec — Structural Measurements Reference checked 2026-10-26

Related: Trend · Plunge · Lineation

View schematic: Trend and plunge: two views of one line

Reservoir geology#

Plunge

The downward inclination of a geological line relative to horizontal, measured in the vertical plane containing the line.

Field context Record trend/plunge in degrees and state the order. A line contained in a plane cannot plunge more steeply than that plane dips. Unoriented cuttings do not establish geographic trend and plunge.

Worked example: trend, plunge and rake

References & related terms

Géologie Québec — Structural Measurements Reference checked 2026-10-26

Related: Trend · Rake · Lineation

View schematic: Trend and plunge: two views of one line

Reservoir geology#

Fault core

The comparatively narrow, strongly deformed part of a fault zone in which displacement is concentrated and original rock relationships may be largely destroyed. It can contain gouge, breccia, cataclasite or multiple slip surfaces.

Field context Core thickness and composition can vary along a fault and through time. A fine-grained core may impede cross-fault flow, but that behaviour must be tested rather than inferred from the name alone.

Field guide: fault core, damage zone and slickenlines

Also called: Core zone

References & related terms

Waldron and Snyder — Faults, fault zones and shear zones Reference checked 2026-10-26

Related: Fault damage zone · Slickenside · Slickenline · Fault gouge · Cataclasite

View schematic: Fault-zone architecture and slip-direction evidence

Reservoir geology#

Fault damage zone

The fractured and otherwise deformed rock flanking a fault core in which earlier rock relationships remain at least partly recognizable. Subsidiary faults, joints, veins, folds and alteration may occur within it.

Field context Fracture intensity commonly changes with distance and lithology, so a damage-zone boundary need not be sharp or symmetric. Enhanced along-zone flow is possible, not automatic.

Field guide: fault core, damage zone and slickenlines

Also called: Damage zone

References & related terms

Waldron and Snyder — Faults, fault zones and shear zones Reference checked 2026-10-26

Related: Fault core · Slickenside · Slickenline · Fault gouge · Cataclasite

View schematic: Fault-zone architecture and slip-direction evidence

Reservoir geology#

Slickenside

A fault or shear surface smoothed or polished by relative movement of the adjoining rock. Linear grooves, scratches or mineral fibres on the surface are described as slickenlines.

Field context A polished surface supports a slip interpretation, but weathering, later mineral growth and repeated movement can modify it. Do not use polish alone to assign displacement magnitude or sense.

Field guide: fault core, damage zone and slickenlines

Also called: Slickensided surface

References & related terms

Waldron and Snyder — Fault kinematics and field evidence Reference checked 2026-10-26

Related: Fault core · Fault damage zone · Slickenline · Fault gouge · Cataclasite

View schematic: Fault-zone architecture and slip-direction evidence

Reservoir geology#

Slickenline

A linear groove, scratch or mineral fibre on a fault surface that records a direction of relative slip within that surface.

Field context A slickenline constrains slip direction but normally has two possible senses. Establish sense and displacement from independent indicators such as steps, offset markers or matched piercing points.

Field guide: fault core, damage zone and slickenlines

Also called: Slickenside lineation, Fault striation

References & related terms

Waldron and Snyder — Fault kinematics and field evidence Reference checked 2026-10-26

Related: Fault core · Fault damage zone · Slickenside · Fault gouge · Cataclasite · Fault separation · Net slip · Piercing point

View schematic: Fault-zone architecture and slip-direction evidence

Reservoir geology#

Fault gouge

Fine-grained, mechanically broken fault rock without primary cohesion. In the BGS rock-classification scheme it contains less than 30% fragments appreciably coarser than a commonly clay-rich matrix and may be strongly foliated.

Field context Classification depends on the scheme and sample condition. Clay-rich gouge may have low permeability across a fault, but mineralogy, fabric, stress and continuity control actual sealing behaviour.

Field guide: fault core, damage zone and slickenlines

Also called: Fault-gouge

References & related terms

British Geological Survey — Rock Classification Scheme: fault-gouge Reference checked 2026-10-26

Related: Fault core · Fault damage zone · Slickenside · Slickenline · Cataclasite

View schematic: Fault-zone architecture and slip-direction evidence

Reservoir geology#

Cataclasite

A cohesive brittle fault rock produced mainly by mechanical fragmentation and grain-size reduction. In the BGS scheme, cataclastic rocks are classified by fragment-to-matrix proportion as protocataclasite, cataclasite or ultracataclasite.

Field context Do not identify cataclasite from fine grain size alone. Primary cohesion and a brittle fragmental texture distinguish it from unconsolidated fault gouge and from ductile, recrystallized mylonite.

Field guide: fault core, damage zone and slickenlines

Also called: Cataclastic rock

References & related terms

British Geological Survey — Rock Classification Scheme: cataclastic rock Reference checked 2026-10-26

Related: Fault core · Fault damage zone · Slickenside · Slickenline · Fault gouge · Ductile shear zone · Mylonite

View schematic: Fault-zone architecture and slip-direction evidence

Reservoir geology#

Joint set

A group of geological joints with similar orientations within the rock volume being described.

Field context Record the spread of strike and dip, spacing and persistence. Similar orientation alone does not establish identical age.

Worked example: joint sets and aperture

Also called: Set of joints

References & related terms

Waldron and Snyder — Geological Structures: Fractures Reference checked 2026-10-26

Related: Geological joint · Fracture aperture

View schematic: Joint sets and normal aperture

Reservoir geology#

Fracture aperture

The local separation between opposing fracture walls. State the measurement direction; geometric aperture is measured normal to the walls.

Field context Distinguish open space from mineral fill and record measurement conditions. A surface opening alone does not establish connected subsurface flow.

Worked example: joint sets and aperture

Also called: Joint aperture

References & related terms

Waldron and Snyder — Geological Structures: Fractures Reference checked 2026-10-26

Related: Geological joint · Joint set · Mineral vein · Crack-seal growth

View schematic: Joint sets and normal aperture

Reservoir geology#

Geological joint

A natural fracture in rock with no appreciable displacement parallel to its surface.

Field context Distinguish geological joints from pipe joints, faults and breaks introduced during drilling or handling. Describe orientation and opening separately.

Worked example: joint sets and aperture

Also called: Rock joint

References & related terms

Waldron and Snyder — Geological Structures: Fractures Reference checked 2026-10-26

Related: Joint set · Fracture aperture

View schematic: Joint sets and normal aperture

Reservoir geology#

Mineral vein

A distinct mineral body occupying a fracture or fissure in rock, commonly formed by precipitation from fluids.

Field context Describe mineral composition, texture, wall relationships and remaining voids. Mineral filling records a geological history but does not establish present-day permeability.

Worked example: fill thickness versus open aperture

Also called: Vein, Mineral-filled fracture

References & related terms

Waldron and Snyder — Fractures: features of vein fills Reference checked 2026-10-26

Related: Crack-seal growth · Fracture aperture · Geological joint

View schematic: Opening, mineral filling and reopening

Reservoir geology#

Crack-seal growth

Vein growth through repeated fracture opening followed by mineral deposition that seals successive openings.

Field context Test this interpretation using preserved growth or inclusion textures. Visible bands alone do not provide an event count, duration or opening rate.

Worked example: fill thickness versus open aperture

Also called: Crack-seal mechanism

References & related terms

Waldron and Snyder — Fractures: features of vein fills Reference checked 2026-10-26

Related: Mineral vein · Fracture aperture

View schematic: Opening, mineral filling and reopening

Reservoir geology#

Ductile shear zone

A tabular or curving zone of concentrated ductile deformation that is narrow relative to its length and commonly offsets older structures without a single through-going brittle fracture.

Field context Map its boundaries, fabrics, lineations and strain gradients. A surface fault may connect downward into a ductile shear zone, and composite brittle–ductile overprints are common.

Field guide: ductile shear zones and mylonitic fabrics

Also called: Shear zone, Ductile deformation zone

References & related terms

Waldron and Snyder — Shear Zones: definition and geometry Reference checked 2026-10-26

Related: Mylonite · S–C fabric · Shear band · Porphyroclast · Dynamic recrystallization · Crystal-plastic deformation · Core-and-mantle structure

View schematic: Ductile shear-zone fabric and brittle–ductile distinction

Reservoir geology#

Mylonite

A cohesive, strongly foliated fault or shear-zone rock whose grain size has been reduced mainly by crystal-plastic deformation and dynamic recrystallization.

Field context Do not classify a fine-grained fault rock as mylonite from grain size alone. Look for a penetrative fabric, recrystallized matrix, stretched grains or ribbons and other ductile microstructures; separate later brittle overprinting.

Field guide: ductile shear zones and mylonitic fabrics

Also called: Mylonitic rock

References & related terms

British Geological Survey — Moine mylonites and dynamic recrystallization Reference checked 2026-10-26

Related: Ductile shear zone · S–C fabric · Shear band · Porphyroclast · Dynamic recrystallization · Crystal-plastic deformation · Core-and-mantle structure · Protomylonite · Ultramylonite

View schematic: Ductile shear-zone fabric and brittle–ductile distinction

Reservoir geology#

S–C fabric

A composite shear-zone fabric containing an oblique penetrative S foliation and C surfaces that lie closer to the shear-zone boundary and concentrate more deformation.

Field context Use the acute-angle relationship only in a correctly oriented section and together with other indicators. Later overprinting, folding or viewing from the opposite side can reverse an apparent shear-sense interpretation.

Field guide: ductile shear zones and mylonitic fabrics

Also called: S-C fabric, C-S fabric, S/C fabric

References & related terms

Waldron and Snyder — C-S foliation and shear-zone kinematics Reference checked 2026-10-26

Related: Ductile shear zone · Mylonite · Shear band

View schematic: Ductile shear-zone fabric and brittle–ductile distinction

Reservoir geology#

Shear band

A narrow, later shear surface or small shear zone that cuts and offsets an earlier foliation; sets of these bands form an oblique C′ fabric in many ductile shear zones.

Field context Record whether the band truly offsets the earlier foliation and preserve sample orientation. Shear bands can support a movement-sense interpretation, but geometry should be cross-checked with independent kinematic indicators.

Field guide: ductile shear zones and mylonitic fabrics

Also called: C′ foliation, C-prime foliation, Extensional crenulation cleavage

References & related terms

Waldron and Snyder — Shear bands and C-prime foliation Reference checked 2026-10-26

Related: Ductile shear zone · Mylonite · S–C fabric

View schematic: Ductile shear-zone fabric and brittle–ductile distinction

Reservoir geology#

Porphyroclast

A relatively large relict mineral grain or grain aggregate that remains within a finer matrix produced as the surrounding rock underwent deformation and grain-size reduction.

Field context Distinguish a surviving porphyroclast from a porphyroblast that grew larger than its matrix. Record mineral, fractures, internal strain, rim or mantle, tails and section orientation before making a shear-sense interpretation. Relict does not mean undeformed: a porphyroclast may fracture or shrink while remaining coarser than its matrix.

Thin-section guide: porphyroclasts and recrystallization

Also called: Relict porphyroclast

References & related terms

British Geological Survey — Mylonitic-rock classification and porphyroclasts Reference checked 2026-10-29

Related: Dynamic recrystallization · Crystal-plastic deformation · Core-and-mantle structure · Mylonite · Protomylonite · Ultramylonite

View schematic: Porphyroblast, porphyroclast and recrystallized mantle

Reservoir geology#

Dynamic recrystallization

Microstructural reworking during ongoing deformation in which new or reorganized grains form and grain boundaries migrate or are replaced, commonly changing grain size and reducing stored crystal strain.

Field context Identify the mineral and observed mechanism rather than treating fine grain size alone as proof. Recrystallized grain size also depends on temperature, stress, water, strain rate and later overprinting.

Thin-section guide: porphyroclasts and recrystallization

Also called: Syntectonic recrystallization

References & related terms

Ocean Drilling Program Leg 176 — Crystal-plastic microstructures and dynamic recrystallization Reference checked 2026-10-26

Related: Porphyroclast · Crystal-plastic deformation · Core-and-mantle structure · Mylonite

View schematic: Porphyroblast, porphyroclast and recrystallized mantle

Reservoir geology#

Crystal-plastic deformation

Permanent deformation accommodated within crystals by processes such as dislocation motion, mechanical twinning and related recovery or recrystallization, without requiring bulk brittle fragmentation.

Field context Look for mineral-specific evidence such as subgrains, deformation twins, undulose extinction and recrystallized grains. Crystal-plastic and brittle microstructures can coexist in a semibrittle zone.

Thin-section guide: porphyroclasts and recrystallization

Also called: Crystal plasticity, Intracrystalline plastic deformation

References & related terms

Ocean Drilling Program Leg 176 — Crystal-plastic structures in Hole 735B Reference checked 2026-10-26

Related: Porphyroclast · Dynamic recrystallization · Core-and-mantle structure · Ductile shear zone · Mylonite · Finite strain · Strain ellipse

View schematic: Porphyroblast, porphyroclast and recrystallized mantle

Reservoir geology#

Core-and-mantle structure

A deformation microstructure in which a relatively coarse, strained relict grain forms the core and is partly or completely surrounded by a mantle of finer recrystallized grains.

Field context Describe core and mantle mineralogy, grain boundaries and section scale. A fine rim may support dynamic recrystallization, but it does not by itself quantify temperature, stress, strain or elapsed time.

Thin-section guide: porphyroclasts and recrystallization

Also called: Mortar structure, Core-mantle structure

References & related terms

Waldron and Snyder — Shear Zones: mortar and core-and-mantle structure Reference checked 2026-10-26

Related: Porphyroclast · Dynamic recrystallization · Crystal-plastic deformation · Mylonite

View schematic: Porphyroblast, porphyroclast and recrystallized mantle

Reservoir geology#

Protomylonite

A mylonitic rock retaining more than 50% porphyroclasts by volume under the British Geological Survey Rock Classification Scheme.

Field context First establish a mylonitic deformation fabric; coarse-grain abundance alone cannot identify the rock. Report the classification scheme, sampling method and uncertainty, especially near a threshold. Porphyroclast volume is not shear strain.

Worked example: classifying a mylonitic rock near a threshold

Also called: Protomylonitic rock

References & related terms

British Geological Survey — Rock Classification Scheme: PROMYL Reference checked 2026-10-26

Related: Mylonite · Porphyroclast · Dynamic recrystallization · Ultramylonite

View schematic: Porphyroclast-volume classification: two end members

Reservoir geology#

Ultramylonite

A mylonitic rock containing less than 10% porphyroclasts by volume under the British Geological Survey Rock Classification Scheme.

Field context First establish a mylonitic deformation fabric; coarse-grain abundance alone cannot identify the rock. Report the classification scheme, sampling method and uncertainty, especially near a threshold. Porphyroclast volume is not shear strain.

Worked example: classifying a mylonitic rock near a threshold

Also called: Ultramylonitic rock

References & related terms

British Geological Survey — Rock Classification Scheme: ULMYL Reference checked 2026-10-26

Related: Mylonite · Porphyroclast · Dynamic recrystallization · Protomylonite

View schematic: Porphyroclast-volume classification: two end members

Hydrogeology & pore systems#

Layered heterogeneity

Spatial variation in a property arranged in successive layers. In groundwater modelling, beds with different hydraulic conductivities can create directional behaviour at the scale of the combined unit, even when each bed is individually isotropic.

Field context State layer continuity, thickness, test direction and boundary conditions. An equivalent value for a one-dimensional experiment is not automatically a calibrated value for flow near a partially penetrating well.

Worked example: conductivity along and across layers

Also called: Stratified heterogeneity

References & related terms

The Groundwater Project — layered conductivity Reference checked 2026-10-26

Field-context reference

Related: Anisotropy · Heterogeneity · Hydraulic conductivity · Equivalent hydraulic conductivity

View schematic: Layer-parallel and layer-normal groundwater flow

Hydrogeology & pore systems#

Equivalent hydraulic conductivity

A conductivity assigned to a simplified medium so that it reproduces the total flow through a specified heterogeneous system under stated boundary conditions. For continuous isotropic layers, purely layer-parallel and layer-normal flow give different equivalent values.

Field context State layer continuity, thickness, test direction and boundary conditions. An equivalent value for a one-dimensional experiment is not automatically a calibrated value for flow near a partially penetrating well.

Worked example: conductivity along and across layers

Also called: Equivalent K

References & related terms

The Groundwater Project — layered conductivity Reference checked 2026-10-26

Field-context reference

Related: Anisotropy · Heterogeneity · Hydraulic conductivity · Layered heterogeneity

View schematic: Layer-parallel and layer-normal groundwater flow

Reservoir geology#

Flute cast

A raised sedimentary feature on a bed underside formed by filling a scoop-shaped scour in the underlying sediment. A typical preserved flute has a bulbous upstream end and fades downstream, providing evidence of flow sense.

Field context Identify the bed underside and retain sample orientation. Distinguish erosional relief from its sediment fill. Loose cuttings cannot preserve a geographic paleoflow bearing.

Worked example: flow sense versus alignment

Also called: Flute mold, Flute mould

References & related terms

University of Alberta — Waldron, Scour structures Reference checked 2026-10-26

Related: Groove cast · Paleocurrent · Turbidite · Load cast · Flame structure

View schematic: Flute casts and groove casts: direction versus axis

Reservoir geology#

Groove cast

An elongate ridge on a bed underside formed when sediment fills a groove cut into the substrate by a dragged object. A straight, uniform groove records an alignment but does not by itself resolve which way along it the object moved.

Field context Identify the bed underside and retain sample orientation. Distinguish erosional relief from its sediment fill. Loose cuttings cannot preserve a geographic paleoflow bearing.

Worked example: flow sense versus alignment

Also called: Groove mold, Groove mould

References & related terms

Peakall et al. (2020) — Flutes and tool marks, Sedimentology Reference checked 2026-10-26

Related: Flute cast · Paleocurrent · Turbidite · Load cast · Flame structure

View schematic: Flute casts and groove casts: direction versus axis

Reservoir geology#

Load cast

A downward bulge at a bed base produced when denser sediment, commonly sand, deforms an underlying softer, less dense sediment before lithification.

Field context Record the contact in section and plan where possible. Shape alone does not establish a paleoflow bearing or the trigger of deformation. Loose cuttings do not preserve bed-scale orientation.

Worked example: describe a deformed bed contact

Also called: Load mold, Load mould

References & related terms

Waldron and Snyder — Geological Structures: a Practical Introduction, Primary Structures Reference checked 2026-10-26

Related: Flame structure · Flute cast · Groove cast · Convolute lamination · Slump fold

View schematic: Load casts and flame structures at a sand–mud contact

Reservoir geology#

Flame structure

A narrow, upward-projecting tongue of mud between downward load structures in an overlying sediment bed, formed during soft-sediment deformation.

Field context Record the contact in section and plan where possible. Shape alone does not establish a paleoflow bearing or the trigger of deformation. Loose cuttings do not preserve bed-scale orientation.

Worked example: describe a deformed bed contact

Also called: Mud flame

References & related terms

Waldron and Snyder — Geological Structures: a Practical Introduction, Primary Structures Reference checked 2026-10-26

Related: Load cast · Flute cast · Groove cast · Convolute lamination · Slump fold

View schematic: Load casts and flame structures at a sand–mud contact

Reservoir geology#

Convolute lamination

Strongly folded or contorted laminae restricted to a sedimentary bed, with the deformation fading toward its bounding, relatively undisturbed layers. It is a descriptive soft-sediment structure; its shape alone does not identify the disturbance mechanism.

Field context Document the bounding beds, internal continuity, recovery and drilling disturbance. Use independent context before inferring movement, trigger or paleoslope; unoriented cuttings cannot preserve this bed-scale geometry.

Worked example: describe folded laminae in core

Also called: Convoluted lamination

References & related terms

IODP Expedition 397 Methods — Deformational structures Reference checked 2026-10-26

Related: Slump fold · Load cast · Flame structure · Dish structure · Pillar structure

View schematic: Convolute lamination and a candidate slump fold

Reservoir geology#

Slump fold

A fold formed by downslope deformation of sediment while it was still soft. Recognition requires evidence for early sediment movement, rather than merely the presence of curved bedding.

Field context Document the bounding beds, internal continuity, recovery and drilling disturbance. Use independent context before inferring movement, trigger or paleoslope; unoriented cuttings cannot preserve this bed-scale geometry.

Worked example: describe folded laminae in core

Also called: Slump folding

References & related terms

IODP Expedition 397 Methods — Deformational structures Reference checked 2026-10-26

Related: Convolute lamination · Load cast · Flame structure

View schematic: Convolute lamination and a candidate slump fold

Reservoir geology#

Dish structure

A dewatering structure expressed by thin, clay-enriched, nearly horizontal to concave-up laminae in sandy or silty sediment. Dishes may interrupt earlier lamination and commonly occur with pillars; they do not by themselves identify the original depositional environment.

Field context Record bed contacts, section orientation and cross-cutting relationships. Distinguish a sedimentary pillar from a burrow, fracture fill or drilling artifact; loose cuttings cannot establish bed-scale geometry.

Worked example: describe dish and pillar geometry

Also called: Dish lamination

References & related terms

Lowe and LoPiccolo (1974), The Characteristics and Origins of Dish and Pillar Structures — original abstract Reference checked 2026-10-27

Related: Pillar structure · Convolute lamination

View schematic: Dish laminae and a pillar

Reservoir geology#

Pillar structure

A steep column or sheet of relatively structureless sediment formed along a localized water-escape pathway in soft sediment. Pillars commonly interrupt dish laminae and may be depleted in fine particles relative to the surrounding sediment.

Field context Record bed contacts, section orientation and cross-cutting relationships. Distinguish a sedimentary pillar from a burrow, fracture fill or drilling artifact; loose cuttings cannot establish bed-scale geometry.

Worked example: describe dish and pillar geometry

Also called: Fluidization pipe, Elutriation pipe

References & related terms

Lowe and LoPiccolo (1974), The Characteristics and Origins of Dish and Pillar Structures — original abstract Reference checked 2026-10-27

Related: Dish structure · Convolute lamination

View schematic: Dish laminae and a pillar

Wellsite geology & samples#

Pleochroism

A change in a mineral’s absorption colour as its orientation to plane-polarized light changes. It is observed with the analyser removed and depends on the section orientation; several grains may be needed to characterize the mineral’s full colour range.

Field context Use a prepared transparent section or grain mount and document the microscope mode, orientation and reference trace. Combine optical evidence with other mineral properties; a hand-lens observation is not an optical-extinction measurement.

Worked example: optical observations and extinction angle

Also called: Pleochroic colour change

References & related terms

Tulane University — Stephen A. Nelson, optical mineralogy lectures Reference checked 2026-10-26

Related: Optical extinction · Extinction angle

View schematic: Absorption colour and crossed-polar extinction

Wellsite geology & samples#

Optical extinction

Darkness of a transparent crystal section under crossed polarizers when its permitted vibration directions align with the polarizer and analyser. In a suitable anisotropic section, extinction recurs at 90° stage intervals. Persistent darkness alone does not uniquely establish isotropy.

Field context Use a prepared transparent section or grain mount and document the microscope mode, orientation and reference trace. Combine optical evidence with other mineral properties; a hand-lens observation is not an optical-extinction measurement.

Worked example: optical observations and extinction angle

Also called: Extinction under crossed polars

References & related terms

Tulane University — Stephen A. Nelson, optical mineralogy lectures Reference checked 2026-10-26

Related: Pleochroism · Extinction angle

View schematic: Absorption colour and crossed-polar extinction

Wellsite geology & samples#

Extinction angle

The angle between a crystallographic reference trace, such as cleavage or elongation, and a vibration direction identified at optical extinction. The measured value depends on section orientation; a single grain need not show the mineral’s maximum diagnostic angle.

Field context Use a prepared transparent section or grain mount and document the microscope mode, orientation and reference trace. Combine optical evidence with other mineral properties; a hand-lens observation is not an optical-extinction measurement.

Worked example: optical observations and extinction angle

Also called: Optical extinction angle

References & related terms

Tulane University — Stephen A. Nelson, optical mineralogy lectures Reference checked 2026-10-26

Related: Pleochroism · Optical extinction

View schematic: Absorption colour and crossed-polar extinction

Reservoir geology#

Thermochronology

The study of rock and mineral temperature histories using time-sensitive records whose preservation changes with temperature, including radiogenic helium retention and fission-track annealing. Dates, other measured properties and kinetic models together constrain thermal evolution; a thermochronological date is not automatically the age of crystallization or sediment deposition.

Field context In a basin study, document the sample, mineral, analytical system and thermal model. Detrital inheritance and later heating can complicate the record; do not substitute a cooling interpretation for a formation age or hydrocarbon-maturity assessment.

Worked example: cooling rate and age interpretation

Also called: Thermochronometry

References & related terms

UCL — Pieter Vermeesch, Geochronology, Chapter 7: Thermochronology Reference checked 2026-10-26

Related: Closure temperature · Radiometric dating · Closed isotopic system

View schematic: An invented cooling interval

Reservoir geology#

Closure temperature

An effective temperature associated with the apparent age of a thermochronometer under an assumed cooling history. For diffusion-controlled systems it depends on diffusion kinetics, effective domain size and geometry, and cooling rate. It summarizes gradual retention behaviour rather than describing a universal, instantaneous switch in a mineral.

Field context In a basin study, document the sample, mineral, analytical system and thermal model. Detrital inheritance and later heating can complicate the record; do not substitute a cooling interpretation for a formation age or hydrocarbon-maturity assessment.

Worked example: cooling rate and age interpretation

Also called: Isotopic closure temperature

References & related terms

Tian et al. (2024) — Rock exhumation inversion, section 3; DOI 10.5194/esurf-12-477-2024 Reference checked 2026-10-26

Related: Thermochronology · Radiometric dating · Closed isotopic system

View schematic: An invented cooling interval

Reservoir geology#

Polarity zone

A rock unit distinguished by its remanent magnetic polarity character. It may record one polarity or a characteristic pattern containing opposite-polarity intervals. It is a material stratigraphic unit: recognizing it does not by itself establish when the magnetization was acquired.

Field context Keep the observed core polarity, proposed chron assignment and independent age constraints separate in the correlation record. A matching pattern is a hypothesis to test.

Worked example: polarity correlation and age control

Also called: Magnetostratigraphic polarity zone, Magnetopolarity zone

References & related terms

North American Stratigraphic Code — Articles 43–46 Reference checked 2026-10-26

Related: Polarity chron · Biostratigraphy · Radiometric dating

View schematic: A polarity pattern needs an age anchor

Reservoir geology#

Polarity chron

The time interval represented by a magnetostratigraphic polarity unit. A chron describes time, whereas a polarity zone describes a body of rock. Assigning a local polarity sequence to a named chron requires correlation with a reference timescale and supporting age evidence.

Field context Keep the observed core polarity, proposed chron assignment and independent age constraints separate in the correlation record. A matching pattern is a hypothesis to test.

Worked example: polarity correlation and age control

Also called: Magnetostratigraphic polarity chron

References & related terms

International Commission on Stratigraphy — Magnetostratigraphic polarity units Reference checked 2026-10-26

Related: Polarity zone · Biostratigraphy · Radiometric dating

View schematic: A polarity pattern needs an age anchor

Petrophysics & log interpretation#

Void ratio

Pore-space volume divided by solid-material volume, e = Vv/Vs. It differs from porosity, whose denominator is the whole sample volume. For the same volume accounting, e = n/(1 − n) and n = e/(1 + e). Void ratio is dimensionless and can exceed one.

Field context State which pores are counted, the sample volume and measurement conditions. Bulk volume may change during drying or compaction; do not mix measurements from different sample states.

Worked example: pore volume, water content and saturation

References & related terms

The Groundwater Project — 3.4 Void ratio Reference checked 2026-10-26

Related: Volumetric water content · Porosity · Fluid saturation · Effective porosity

View schematic: One sample, four different volume ratios

Petrophysics & log interpretation#

Volumetric water content

Water volume divided by the bulk volume of a porous sample, θ = Vw/Vt. Water saturation instead divides water volume by pore volume. With matching pore-volume conventions, θ = n Sw. Volumetric water content is dimensionless and is distinct from a water-to-solid mass ratio.

Field context State which pores are counted, the sample volume and measurement conditions. Bulk volume may change during drying or compaction; do not mix measurements from different sample states.

Worked example: pore volume, water content and saturation

Also called: Volumetric moisture content

References & related terms

The Groundwater Project — 3.5 Volumetric moisture content Reference checked 2026-10-26

Related: Void ratio · Porosity · Fluid saturation · Effective porosity

View schematic: One sample, four different volume ratios

Hydrogeology & pore systems#

Sorption

Transfer of a substance from a fluid to a solid surface or into another phase. The term includes surface adsorption and uptake into a phase by absorption. In groundwater, reversible sorption can delay transport without destroying the substance; it must be distinguished from degradation.

Field context Report water chemistry, solid composition, concentration range and equilibration time. Do not transfer a laboratory coefficient to a different geological interval without checking those conditions.

Worked example: water speed versus solute migration

References & related terms

The Groundwater Project — 12.3 Reactions and retardation Reference checked 2026-10-26

Related: Sorption distribution coefficient · Retardation factor · Average linear groundwater velocity · Effective porosity

View schematic: Water movement and reversible sorption

Hydrogeology & pore systems#

Sorption distribution coefficient Kd

Ratio of sorbed concentration per dry mass of solid to dissolved concentration per volume of water at specified conditions: Kd = Cs/Cw. Common units are L/kg. A constant Kd describes a linear equilibrium sorption model; it is not a universal material constant or the dimensionless mineral–melt partition coefficient.

Field context Report water chemistry, solid composition, concentration range and equilibration time. Do not transfer a laboratory coefficient to a different geological interval without checking those conditions.

Worked example: water speed versus solute migration

Also called: Solid–water distribution coefficient

References & related terms

US EPA (1999), Understanding Variation in Partition Coefficient, Kd, Values, Volume II, section 2 Reference checked 2026-10-26

Related: Sorption · Retardation factor · Average linear groundwater velocity · Effective porosity

View schematic: Water movement and reversible sorption

Hydrogeology & pore systems#

Retardation factor

Dimensionless ratio of average pore-water speed to the migration speed of a solute under a stated transport model. For saturated, homogeneous material with instantaneous reversible linear sorption and uniformly accessible pores, R = 1 + ρb Kd/n, using dry bulk density ρb and matching porosity n. Delay alone does not imply mass destruction.

Field context Report water chemistry, solid composition, concentration range and equilibration time. Do not transfer a laboratory coefficient to a different geological interval without checking those conditions.

Worked example: water speed versus solute migration

Also called: Solute retardation factor

References & related terms

The Groundwater Project — 7.3 Phosphorus fate, retardation equation Reference checked 2026-10-26

Related: Sorption · Sorption distribution coefficient · Average linear groundwater velocity · Effective porosity · Mechanical dispersion · Dispersivity

View schematic: Water movement and reversible sorption

Wellsite geology & samples#

Crystal twinning

An oriented intergrowth of crystal domains related by a specific symmetry operation that is not a symmetry operation of the individual crystal. Twins can form during growth, structural transformation or deformation; the visible pattern alone does not establish which process occurred.

Field context Record the observed pattern separately from the proposed mineral name. Retain an unresolved identification when preparation, alteration or orientation prevents a useful comparison.

Worked observations: identifying feldspar twins

Also called: Twinning (mineral)

References & related terms

Tulane University — Stephen A. Nelson, Twinning in Crystals Reference checked 2026-10-27

Related: Polysynthetic twinning · Microcline · Feldspar · Optical extinction

View schematic: Feldspar twin patterns and an unresolved grain

Wellsite geology & samples#

Polysynthetic twinning

Repeated twinning with parallel composition surfaces separating successive crystal domains. Albite-law twins are common in plagioclase and may appear as alternating bands under crossed polarizers. The bands represent changes in crystallographic orientation, not a stack of sedimentary layers.

Field context Record the observed pattern separately from the proposed mineral name. Retain an unresolved identification when preparation, alteration or orientation prevents a useful comparison.

Worked observations: identifying feldspar twins

Also called: Repeated lamellar twinning

References & related terms

Tulane University — Stephen A. Nelson, Types of Twinning Reference checked 2026-10-27

Related: Crystal twinning · Microcline · Feldspar · Optical extinction · Mineral exsolution · Perthite · Compositional zoning · Oscillatory zoning

Additional schematic: Plagioclase zoning: endpoints and internal variation

View schematic: Feldspar twin patterns and an unresolved grain

Wellsite geology & samples#

Microcline

A triclinic potassium feldspar with ideal composition KAlSi3O8, found in many granitic, pegmatitic and metamorphic rocks. Combined albite- and pericline-law twins can produce a characteristic cross-hatched, or tartan, pattern in suitable sections. Microcline is a mineral species within the feldspar group.

Field context Record the observed pattern separately from the proposed mineral name. Retain an unresolved identification when preparation, alteration or orientation prevents a useful comparison.

Worked observations: identifying feldspar twins

References & related terms

National Museum of Natural History, Sofia — Microcline Reference checked 2026-10-27

Related: Crystal twinning · Polysynthetic twinning · Feldspar · Optical extinction

View schematic: Feldspar twin patterns and an unresolved grain

Geophysics & seismic#

Seismic wavelength

Spatial length of one cycle of a seismic wave. For a specified wave mode and frequency in a uniform medium, wavelength λ = v/f, where v is propagation speed and f is frequency. A broadband seismic pulse contains multiple wavelengths.

Field context Specify the wave mode, target-interval velocity, frequency estimate and resolution criterion. Seismic resolution and along-tool logging resolution describe different measurement supports.

Worked example: wavelength, bed separability and sampling

Also called: Wavelength (seismic)

References & related terms

UBC EOSC 350 — Vertical resolution Reference checked 2026-10-27

Related: Vertical seismic resolution · Wavelet · Seismic tuning

View schematic: Wavelength and a quarter-wavelength separability estimate

Geophysics & seismic#

Vertical seismic resolution

Ability to distinguish reflections from vertically separated interfaces, such as a bed’s top and base. A quarter wavelength is a common idealized separability estimate; actual performance depends on the wavelet, bandwidth, noise and processing. Detecting a thin-bed response does not necessarily resolve its two boundaries.

Field context Specify the wave mode, target-interval velocity, frequency estimate and resolution criterion. Seismic resolution and along-tool logging resolution describe different measurement supports. Compare a calculated summed wavelet response with interface times before equating trace extrema with bed boundaries. Sample spacing alone does not establish boundary separability.

Worked example: two interfaces and a summed seismic trace

Also called: Seismic vertical resolution

References & related terms

Takahashi (2022), Vertical resolution and seismic data interpretation, DOI 10.3124/segj.75.79 Reference checked 2026-10-29

Field-context reference

Related: Seismic wavelength · Wavelet · Seismic tuning · Sampling aliasing · Nyquist frequency

View schematic: Wavelength and a quarter-wavelength separability estimate

Sedimentology & sedimentary rocks#

Firmground

A cohesive, partly consolidated sediment substrate that was firm but not lithified when organisms colonized it. Compaction and dewatering can produce such material; later erosion may expose it for renewed burrowing. Interpret its former condition from preserved relationships rather than present rock hardness.

Field context Record the contact, trace walls, fill, cross-cutting order and cement evidence separately. Substrate-controlled traces do not alone determine water depth or the duration of a hiatus.

Worked example: firmground or hardground?

Also called: Firm ground

References & related terms

University of Kansas Ichnology — Models: substrate consistency Reference checked 2026-10-27

Related: Hardground · Trace fossil · Bioturbation · Condensed section

View schematic: Firm and lithified substrates at colonization

Sedimentology & sedimentary rocks#

Hardground

A sedimentary surface or substrate that was cemented or lithified while exposed to colonization, commonly at the sea floor. Borings and attached encrusting organisms can provide evidence of an already hard substrate. A hard bed produced by later burial cementation alone does not establish a depositional hardground.

Field context Record the contact, trace walls, fill, cross-cutting order and cement evidence separately. Substrate-controlled traces do not alone determine water depth or the duration of a hiatus.

Worked example: firmground or hardground?

Also called: Hard ground

References & related terms

SEPM STRATA — Ichnofacies: substrate character Reference checked 2026-10-27

Related: Firmground · Trace fossil · Bioturbation · Condensed section

View schematic: Firm and lithified substrates at colonization

Reservoir geology#

Rock cleavage

A secondary planar fabric that gives a rock a tendency to split along repeated surfaces. Aligned minerals and other fabric elements can create this directional weakness. It is a rock-scale structure, distinct from the crystallographic cleavage of an individual mineral and from original sedimentary bedding.

Field context Record the observation scale, section orientation and overprinting evidence. A two-dimensional trace is not a complete plane orientation; relative fabric order alone does not establish a numerical age or a separate regional tectonic event.

Worked fabric example: rock cleavage and crenulation

Also called: Cleavage (rock), Tectonic cleavage

References & related terms

Samuele Papeschi, EGU — Features from the field: Foliation Reference checked 2026-10-27

Related: Crenulation cleavage · Mineral cleavage · Crenulation lineation · Fold · Fissility

View schematic: Earlier foliation, later cleavage and hinge lineation

Reservoir geology#

Crenulation cleavage

A planar fabric defined by the closely repeated axial surfaces of small folds in an earlier foliation. It records overprinting of a pre-existing fabric; the aligned fold hinges instead define a crenulation lineation. The planar and linear features should be described and measured separately.

Field context Record the observation scale, section orientation and overprinting evidence. A two-dimensional trace is not a complete plane orientation; relative fabric order alone does not establish a numerical age or a separate regional tectonic event.

Worked fabric example: rock cleavage and crenulation

Also called: Crenulation foliation

References & related terms

Waldron and Snyder, University of Alberta — Fabrics Reference checked 2026-10-27

Additional interpretation reference

Related: Rock cleavage · Mineral cleavage · Crenulation lineation · Fold

View schematic: Earlier foliation, later cleavage and hinge lineation

Reservoir geology#

Current ripple

A small sediment bedform produced by predominantly one-way flow. A typical migrating current ripple has a longer, gentler upstream stoss flank and a shorter, steeper downstream lee flank. Its preserved shape and internal lamination can help interpret local transport, but asymmetry alone does not prove a purely unidirectional origin.

Field context Describe the profile, crest pattern, section orientation and surrounding facies before assigning a process. Bed slope and combined wave–current flow affect ripple geometry; detached cuttings rarely preserve the required spatial context.

Worked ripple example: flow axis versus flow direction

Also called: Unidirectional current ripple

References & related terms

Samuele Papeschi, EGU — Features from the field: Ripple Marks Reference checked 2026-10-27

Additional interpretation reference

Related: Wave ripple · Cross-bedding · Lamination · Paleocurrent

View schematic: Ripple profiles: current direction and oscillation axis

Reservoir geology#

Wave ripple

A small sediment bedform generated by wave-driven oscillatory motion near the bed. Approximately symmetric profiles are a familiar end member, but wave-generated ripples may also be asymmetric. Crest orientation can constrain an oscillation axis; it does not, by itself, identify a single net sediment-transport direction.

Field context Describe the profile, crest pattern, section orientation and surrounding facies before assigning a process. Bed slope and combined wave–current flow affect ripple geometry; detached cuttings rarely preserve the required spatial context.

Worked ripple example: flow axis versus flow direction

Also called: Wave-formed ripple, Oscillation ripple

References & related terms

National Park Service — Ancient Ripple Marks Reference checked 2026-10-27

Additional interpretation reference

Related: Current ripple · Cross-bedding · Lamination · Paleocurrent · Combined flow · Hummocky cross-stratification

View schematic: Ripple profiles: current direction and oscillation axis

Reservoir geology#

Clast-supported texture

A fabric in which touching coarse fragments form the framework of a sediment or rock. Finer material, cement or pores may occupy spaces between those fragments. The description concerns contact relationships; it does not specify a unique transport process or imply that the rock has high permeability.

Field context Record the coarse population, contact pattern and finer material separately. A small cut surface may miss contacts outside its plane; loose cuttings do not preserve the original contact network. In the guide’s ideal geometry, two touching spheres of radius 5 mm have separated circular intersections on a plane 3 mm from their centres: each section radius is 4 mm, leaving a 2 mm apparent gap. A missing contact in one section therefore does not prove separation in three dimensions.

Worked example: describe the supporting fabric

Also called: Clast support

References & related terms

IODP Expedition 350 Methods — clast supported versus matrix supported Reference checked 2026-10-31

Additional interpretation reference

Related: Matrix-supported texture · Matrix · Breccia · Conglomerate

Additional schematic: A cut plane can miss a grain contact

View schematic: Clast support versus matrix support

Reservoir geology#

Matrix-supported texture

A fabric in which larger fragments are dispersed within surrounding finer material rather than forming the main touching framework. Matrix is relative to the larger fragments and need not be clay. The term describes the preserved arrangement; a depositional mechanism requires additional evidence.

Field context Record the coarse population, contact pattern and finer material separately. A small cut surface may miss contacts outside its plane; loose cuttings do not preserve the original contact network.

Worked example: describe the supporting fabric

Also called: Matrix support

References & related terms

IODP Expedition 350 Methods — clast supported versus matrix supported Reference checked 2026-10-27

Additional interpretation reference

Related: Clast-supported texture · Matrix · Breccia · Conglomerate

View schematic: Clast support versus matrix support

Reservoir geology#

Mineral replacement

Conversion of a pre-existing mineral into another mineral or mineral assemblage in the space it occupied. Many fluid-mediated replacements involve dissolution of the parent coupled to precipitation of a product. The original external form may be preserved or lost; replacement is not simply the filling of an initially empty pore.

Field context Record present mineral identification, external shape and evidence for the precursor separately. Disaggregated cuttings may not retain the relationships needed to distinguish replacement from a coating or pore-filling cement.

Worked example: inherited shape and present mineral identity

Also called: Replacement of minerals

References & related terms

Putnis (2009) — Mineral Replacement Reactions Reference checked 2026-10-27

Additional interpretation reference

Related: Pseudomorph · Diagenesis · Dolomitization · Calcite

View schematic: Replacement with an inherited outline

Reservoir geology#

Pseudomorph

A mineral or mineral aggregate that retains the recognizable external form of a different, earlier mineral. Its outline therefore records a precursor rather than necessarily identifying the material now present. A replacement pseudomorph combines changed mineral identity with inherited shape; the preserved form alone does not establish the reaction mechanism.

Field context Record present mineral identification, external shape and evidence for the precursor separately. Disaggregated cuttings may not retain the relationships needed to distinguish replacement from a coating or pore-filling cement.

Worked example: inherited shape and present mineral identity

Also called: Mineral pseudomorph

References & related terms

Smithsonian Q?rius — Pseudomorphic Minerals Reference checked 2026-10-27

Additional interpretation reference

Related: Mineral replacement · Diagenesis · Dolomitization · Calcite · Bastite · Mesh texture

Additional schematic: Bastite and mesh: inherited texture clues

View schematic: Replacement with an inherited outline

Hydrogeology & pore systems#

Isotropy

Independence of a specified material property from direction at a stated location and observation scale. Hydraulic isotropy means the same conductivity in every direction; it does not require that conductivity be identical at other locations, or that electrical and elastic properties also be isotropic.

Field context State axes, scale and the property being tested. Equal horizontal conductivities alone do not establish three-dimensional isotropy. A head map without directional conductivity information may not determine the flow direction.

Worked example: head-gradient and flow directions

Also called: Isotropic property

References & related terms

Groundwater Project — spatial and directional variation of conductivity Reference checked 2026-10-27

Additional interpretation reference

Related: Hydraulic conductivity tensor · Anisotropy · Hydraulic conductivity · Hydraulic gradient

View schematic: Head-drop direction and Darcy flux

Hydrogeology & pore systems#

Hydraulic conductivity tensor

The directional conductivity coefficients that map a hydraulic-head gradient to Darcy flux through q = −K ∇h. For conventional saturated Darcy flow, K is a symmetric second-rank tensor with length-per-time units. In principal coordinates it is diagonal; in rotated coordinates off-diagonal coefficients generally couple gradient and flux components.

Field context State axes, scale and the property being tested. Equal horizontal conductivities alone do not establish three-dimensional isotropy. A head map without directional conductivity information may not determine the flow direction.

Worked example: head-gradient and flow directions

Also called: Conductivity tensor for groundwater

References & related terms

Freeze and Cherry (1979), Groundwater, chapter 2 — generalized Darcy law Reference checked 2026-10-27

Additional interpretation reference

Related: Isotropy · Anisotropy · Hydraulic conductivity · Hydraulic gradient

View schematic: Head-drop direction and Darcy flux

Reservoir geology#

Detrital zircon

A zircon grain incorporated into sediment as a transported mineral particle derived from pre-existing material. Its interpreted U–Pb age can record a source-rock event predating deposition. Grain-age populations inform sediment-source studies; a reliable youngest component may limit the age of the containing deposit.

Field context Keep sample position, grain selection, analytical uncertainties and the dated event explicit. Younger contamination or disturbed isotopic systems can invalidate an apparent youngest age; an age bound is not a direct formation-top pick.

Worked example: a grain-age bound and an overlying ash

Also called: Detrital zircon grain

References & related terms

University of Saskatchewan Physical Geology — Isotopic Dating Methods Reference checked 2026-10-27

Additional interpretation reference

Related: Maximum depositional age · Detrital · Radiometric dating · Chronostratigraphic correlation

View schematic: A maximum depositional age is a bound

Reservoir geology#

Maximum depositional age MDA

An older numerical-age limit on deposition, commonly estimated from the youngest defensible detrital mineral age. A sediment containing a valid pre-depositional grain cannot have formed before that grain. An MDA constrains deposition to the same age or younger; it does not by itself identify the actual depositional age.

Field context Keep sample position, grain selection, analytical uncertainties and the dated event explicit. Younger contamination or disturbed isotopic systems can invalidate an apparent youngest age; an age bound is not a direct formation-top pick.

Worked example: a grain-age bound and an overlying ash

Also called: Maximum age of deposition

References & related terms

Johnstone, Schwartz and Holm-Denoma (2019), USGS publication record Reference checked 2026-10-27

Additional interpretation reference

Related: Detrital zircon · Detrital · Radiometric dating · Chronostratigraphic correlation

View schematic: A maximum depositional age is a bound

Reservoir geology#

Flaser bedding

Heterolithic bedding in which rippled sand contains discontinuous streaks of mud, commonly preserved in ripple troughs while crests remain partly or wholly uncovered. It describes the arrangement of contrasting sediment fractions, rather than a unique depositional environment. More continuous mud layers approach wavy bedding.

Field context Describe sand–mud continuity on intact material before inferring tidal processes or reservoir connectivity. Loose cuttings rarely retain the spatial relationships needed to identify this bedding reliably.

Worked core descriptions: flaser and lenticular bedding

Also called: Flaser stratification

References & related terms

Kansas Geological Survey — Lawrence Formation results Reference checked 2026-10-27

Additional interpretation reference

Related: Lenticular bedding · Lamination · Current ripple · Facies

View schematic: Flaser and lenticular bedding: trace the contrasting material

Reservoir geology#

Lenticular bedding

Heterolithic bedding with ripple-derived sand lenses within a predominantly muddy deposit. The lenses may be isolated or connected locally; their thickness and continuity are descriptive features. This bedding-scale term does not refer to every lens-shaped sandstone body or channel fill.

Field context Describe sand–mud continuity on intact material before inferring tidal processes or reservoir connectivity. Loose cuttings rarely retain the spatial relationships needed to identify this bedding reliably.

Worked core descriptions: flaser and lenticular bedding

Also called: Lenticular stratification

References & related terms

Kansas Geological Survey — Waverly tidal-flat sedimentology Reference checked 2026-10-27

Additional interpretation reference

Related: Flaser bedding · Lamination · Current ripple · Facies

View schematic: Flaser and lenticular bedding: trace the contrasting material

Reservoir geology#

Fault separation

The offset between corresponding cutoff traces of a displaced marker, measured in a stated direction or section. Separation describes geometry; a single displaced planar marker generally does not determine the fault-slip vector.

Field context Name the marker, section and measurement direction. An apparent normal or reverse separation need not establish the sense of slip. Down-dip distance is not vertical displacement; geographic components require fault attitude and an explicit reference block.

Worked example: fault-plane versus vertical displacement

Also called: Separation (fault geometry)

References & related terms

Waldron and Snyder — Fault geometry and kinematics Reference checked 2026-10-29

Additional interpretation reference

Related: Net slip · Piercing point · Fault · Slickenline · Rake

View schematic: One marker offset, multiple possible slip vectors

Reservoir geology#

Net slip

The resultant relative displacement between formerly adjacent points on opposite sides of a fault. It has magnitude, orientation and sense, and can be resolved into strike-parallel and dip-parallel components within the fault plane.

Field context State which block is the reference. Net displacement is not necessarily the total distance travelled through a history of changing slip directions. Down-dip distance is not vertical displacement; geographic components require fault attitude and an explicit reference block.

Worked example: fault-plane versus vertical displacement

Also called: Net fault slip, Fault-slip vector

References & related terms

University of Michigan — Fault geometries and displacement Reference checked 2026-10-29

Additional interpretation reference

Related: Fault separation · Piercing point · Fault · Slickenline · Rake

View schematic: One marker offset, multiple possible slip vectors

Reservoir geology#

Piercing point

The point where an identifiable geological line intersects a fault surface. A securely matched pair on opposite fault walls can constrain net displacement; the line may be defined by the intersection of two geological surfaces.

Field context Confirm that both points represent the same original feature. A bed cutoff seen in one section is not automatically a uniquely matched piercing point in three dimensions.

Worked example: fault separation versus net slip

Also called: Fault piercing point

References & related terms

Waldron and Snyder — Fault geometry and kinematics Reference checked 2026-10-27

Additional interpretation reference

Related: Fault separation · Net slip · Fault · Slickenline · Rake

View schematic: One marker offset, multiple possible slip vectors

Reservoir geology#

Mineral–melt partition coefficient

The equilibrium concentration of an element in a specified mineral divided by its concentration in the coexisting melt, using the same concentration basis. The ratio is dimensionless; reversing the phase order gives its reciprocal.

Field context State the element, mineral, melt composition and conditions. A mineral value is not the bulk coefficient of a mixed rock; do not confuse this ratio with a fluid–solid sorption coefficient that carries units. For mass-based concentrations, convert mineral volume proportions to mass fractions using their densities before calculating a bulk coefficient.

Worked example: convert mineral volume to mass fractions

Also called: Mineral-melt distribution coefficient

References & related terms

Imperial College London — Distribution coefficients Reference checked 2026-10-27

Additional interpretation reference

Related: Compatible element · Incompatible element · Feldspar · Partial melting · Fractional crystallization

View schematic: Partition coefficient compares concentrations, not inventories

Reservoir geology#

Compatible element

An element with a mineral/melt concentration ratio greater than one for the specified equilibrium pair. It is more concentrated in that mineral than in the coexisting melt; compatibility is conditional on the phases and conditions.

Field context Greater concentration does not mean that most of the element mass resides in the mineral. The masses of the mineral and melt must also be known. Bulk compatibility can cross the value one when mineral mass proportions change, even if each mineral coefficient stays fixed. State whether the label refers to one mineral or to the complete solid assemblage.

Worked example: a bulk compatibility threshold

Also called: Compatible trace element

References & related terms

Peate and Hawkesworth (2005) — Element partitioning, section 2.4.1 Reference checked 2026-10-27

Additional interpretation reference

Related: Mineral–melt partition coefficient · Incompatible element · Feldspar · Partial melting · Fractional crystallization

Additional schematic: Bulk compatibility depends on mineral proportions

View schematic: Partition coefficient compares concentrations, not inventories

Reservoir geology#

Incompatible element

An element with a mineral/melt concentration ratio less than one for the specified equilibrium pair. It is more concentrated in the melt than in that mineral. An element can be incompatible in one mineral and compatible in another.

Field context Name the mineral or solid assemblage. An incompatible element need not be completely excluded from crystals, and a concentration ratio alone does not determine the degree of melting. Bulk compatibility can cross the value one when mineral mass proportions change, even if each mineral coefficient stays fixed. State whether the label refers to one mineral or to the complete solid assemblage.

Worked example: a bulk compatibility threshold

Also called: Incompatible trace element

References & related terms

Peate and Hawkesworth (2005) — Element partitioning, section 2.4.1 Reference checked 2026-10-27

Additional interpretation reference

Related: Mineral–melt partition coefficient · Compatible element · Feldspar

Additional schematic: Bulk compatibility depends on mineral proportions

View schematic: Partition coefficient compares concentrations, not inventories

Reservoir geology#

Fossil time averaging

Combining remains of organisms from different times within one fossil assemblage or sample. Accumulation, sediment mixing and the sampling interval can reduce the time resolution of the resulting record; physical association alone does not establish that the organisms lived together.

Field context Distinguish natural mixing from pooling separate sample intervals. The oldest-to-youngest age span and the distribution of specimen ages describe different aspects of temporal resolution.

Fossil time averaging: a worked assemblage example

Also called: Time averaging of fossils, Time-averaged fossil assemblage

References & related terms

Kansas Geological Survey Bulletin 233 — Ancient communities, Time averaging Reference checked 2026-10-27

Additional interpretation reference

Related: Death assemblage · Reworked fossil · Biostratigraphy · Fossil disarticulation

View schematic: One sample can contain several death times

Reservoir geology#

Death assemblage

An accumulation of remains of dead organisms, commonly shells or other durable skeletal parts. It differs from a census of living organisms and may combine multiple generations, preservation histories or source habitats; it need not already be lithified or ancient.

Field context Record which parts and taxa were counted, preservation, sample position and collection method. A modern shell accumulation can supply a longer ecological record, but is not automatically a faithful count of the present living community.

Fossil time averaging: a worked assemblage example

Also called: Dead assemblage

References & related terms

Paleontological Research Institution — Live-Dead Analysis (2025) Reference checked 2026-10-27

Additional interpretation reference

Related: Fossil time averaging · Reworked fossil · Biostratigraphy · Fossil disarticulation

View schematic: One sample can contain several death times

Hydrogeology & pore systems#

Mechanical dispersion

Spreading of a dissolved substance caused by differences in water velocity and flow paths within a porous medium. Spreading parallel to the mean flow is longitudinal; spreading perpendicular to it is transverse. This mechanism is distinct from molecular diffusion, although transport models commonly combine their contributions.

Field context Use the groundwater-transport meaning here, not seismic wave dispersion. Record the observation scale and flow direction; apparent spreading in a model can also reflect its numerical discretization.

Solute spreading: velocity, dispersivity and units

Also called: Mechanical solute dispersion

References & related terms

The Groundwater Project — 12.2 Mass Transport in Groundwater Reference checked 2026-10-27

Additional interpretation reference

Related: Dispersivity · Average linear groundwater velocity · Darcy flux · Retardation factor · Molecular diffusion

View schematic: Solute movement and spreading are different quantities

Hydrogeology & pore systems#

Dispersivity

A length parameter used to represent mechanical spreading in a porous-medium transport model. In a common linear approximation, multiplying longitudinal or transverse dispersivity by average pore-water speed gives the corresponding mechanical dispersion coefficient, with units of length squared per time.

Field context State direction, units, model assumptions and observation scale. Dispersivity is not hydraulic conductivity or a universal constant transferable unchanged from a laboratory column to a heterogeneous aquifer.

Solute spreading: velocity, dispersivity and units

Also called: Dispersion length

References & related terms

Penn State CE 574 — 6.4 Dispersion Reference checked 2026-10-27

Additional interpretation reference

Related: Mechanical dispersion · Average linear groundwater velocity · Darcy flux · Retardation factor · Molecular diffusion

View schematic: Solute movement and spreading are different quantities

Wellsite geology & samples#

Mineral exsolution

Separation of an initially homogeneous mineral solid solution into two or more solid phases of different composition as conditions change. Atomic redistribution within the solid can produce lamellae or other intergrowths; melting is not required. Alkali feldspar unmixing into sodium-rich and potassium-rich domains is a common example.

Field context This entry concerns minerals, not gas coming out of a fluid. Distinguish compositional domains from crystal twins, and document the analytical resolution. Texture alone does not determine a cooling rate.

Feldspar intergrowths: composition, twins and texture

Also called: Solid-state unmixing

References & related terms

Dutrow and Mogk — Modeling Exsolution and Perthite Formation Reference checked 2026-10-27

Additional interpretation reference

Related: Perthite · Feldspar · Polysynthetic twinning · Mineral replacement · Solvus · Lever rule

View schematic: Solid-state unmixing in alkali feldspar

Wellsite geology & samples#

Perthite

An intergrowth of sodium-rich feldspar within a potassium-rich feldspar host. It commonly develops through exsolution of an earlier alkali-feldspar solid solution. Fine lamellae may require microscopy to resolve, and later fluid-mediated alteration can modify the original intergrowth.

Field context Use a texture description with the host and included phases identified. Alternating optical brightness alone does not establish their compositions. Preserve evidence of irregular patches, pores or cross-cutting alteration when interpreting the texture.

Feldspar intergrowths: composition, twins and texture

Also called: Perthitic intergrowth

References & related terms

Petrishcheva et al. (2020) — Spinodal decomposition in alkali feldspar Reference checked 2026-10-27

Additional interpretation reference

Related: Mineral exsolution · Feldspar · Polysynthetic twinning · Mineral replacement · Solvus · Lever rule

View schematic: Solid-state unmixing in alkali feldspar

Wellsite geology & samples#

Ichnofabric

The preserved sediment fabric produced by organism activity, considered together with the primary structures that remain. Description includes recognizable traces and the extent to which biological reworking has modified bedding. An intensity index summarizes one aspect of the fabric; it does not identify the organisms or replace a description of their traces.

Field context Record the observation surface, surviving lamination, burrow geometry and any drilling disturbance. Retain the named index scheme and its legend; different published numerical scales are not interchangeable. Preserve uncertainty at category boundaries: under the Expedition 403 scheme, an estimated disturbed fraction of 28–34% spans codes 1 and 2 because the boundary is 30%. Record the estimate range and scheme instead of treating an averaged code as a measured percentage.

Reading burrowed sediment: fabric, index and environment

Also called: Biogenic sediment fabric

References & related terms

IODP Expedition 382 methods — Bioturbation Reference checked 2026-10-31

Additional interpretation reference

Related: Ichnofacies · Bioturbation · Trace fossil · Lamination · Firmground · Hardground

View schematic: From core fabric to environmental interpretation

Wellsite geology & samples#

Ichnofacies

A recurring association of trace fossils used as a model for interpreting conditions in which organisms interacted with sediment. Trace types, their diversity and their relative abundance can reflect several environmental controls, including substrate, oxygenation, salinity and energy. An ichnofacies is an assemblage-level interpretation, not simply the name of one burrow or a fixed water-depth band.

Field context Test the association against lithology and stratigraphic context. Shared traces can occur in different ichnofacies, and similar associations may form at different depths. Do not assign an environment from a bioturbation score alone.

Reading burrowed sediment: fabric, index and environment

Also called: Trace-fossil facies

References & related terms

Kentucky Geological Survey — Ichnofacies (archived educational resource) Reference checked 2026-10-27

Additional interpretation reference

Related: Ichnofabric · Bioturbation · Trace fossil · Lamination · Firmground · Hardground

View schematic: From core fabric to environmental interpretation

Reservoir geology#

Finite strain

The change in shape and size between a specified initial configuration and a final configuration, separated from rigid-body translation and rotation. It describes the net result over that interval; it does not uniquely specify the sequence of deformation increments or the time taken.

Field context State the reference configuration and strain measure. A final marker shape is insufficient to recover a unique strain history, strain rate or stress. Initial shape and the extent to which a marker followed its surrounding rock need independent support.

Worked strain example: shape ratio versus area change

Also called: Accumulated strain

References & related terms

Waldron and Snyder — Kinematic Analysis and Strain Reference checked 2026-10-27

Additional interpretation reference

Related: Strain ellipse · Stretching lineation · Crystal-plastic deformation · Ductile shear zone

View schematic: Equal shape ratio does not mean equal area change

Reservoir geology#

Strain ellipse

The ellipse produced by homogeneous deformation of an initially circular marker in a two-dimensional material plane. For an initial unit-radius circle, the major and minor semiaxes give the maximum and minimum principal stretches in that plane. Their ratio describes distortion but does not by itself determine area change.

Field context An elliptical grain is not automatically a strain ellipse: its initial shape and mechanical behaviour may be unknown. State the section orientation. A single two-dimensional ellipse does not establish the complete three-dimensional strain ellipsoid.

Worked strain example: shape ratio versus area change

Also called: Finite strain ellipse

References & related terms

Waldron and Snyder — Kinematic Analysis and Strain Reference checked 2026-10-27

Additional interpretation reference

Related: Finite strain · Stretching lineation · Crystal-plastic deformation · Ductile shear zone

View schematic: Equal shape ratio does not mean equal area change

Geophysics & seismic#

Sampling aliasing

Ambiguity introduced when distinct continuous signals produce the same sampled values. In regularly sampled geophysical records, signal content above the Nyquist limit can appear at lower frequencies. Spatial undersampling can likewise make wavelength or apparent arrival direction ambiguous.

Field context Check acquisition spacing and filtering before interpreting a smooth curve. Adding interpolated points to an already aliased single time series does not identify the original signal without additional information.

Worked sampling example: two signals, identical samples

Also called: Aliasing, Frequency aliasing

References & related terms

University of British Columbia — Geophysical Signals and Data Processing Reference checked 2026-10-27

Additional interpretation reference

Related: Nyquist frequency · Seismic trace · Vertical seismic resolution

View schematic: Different signals can have identical samples

Geophysics & seismic#

Nyquist frequency

Half the sampling frequency for uniform time sampling: fN = 1/(2Δt), where Δt is the sample interval in seconds and fN is in hertz. It is a sampling boundary, not the dominant signal frequency or a guarantee of usable instrument bandwidth or geological resolution.

Field context For an unknown-phase, band-limited signal, keep its highest retained frequency below this boundary and allow room for a real filter transition. Exactly two samples per cycle can fail: a sine wave sampled only at its zero crossings is invisible.

Worked sampling example: two signals, identical samples

Also called: Folding frequency

References & related terms

University of British Columbia — Geophysical Signals and Data Processing Reference checked 2026-10-27

Additional interpretation reference

Related: Sampling aliasing · Seismic trace · Vertical seismic resolution

View schematic: Different signals can have identical samples

Reservoir geology#

Mechanical compaction

Reduction of sediment or rock bulk volume through grain rearrangement, rotation, bending, breakage or deformation. It tightens the framework without requiring dissolution at grain contacts; pressure solution is a separate chemical compaction mechanism.

Field context Describe bent mica, collapsed grains or tighter packing before inferring a history. Pore pressure, grain strength and early cement affect compaction; burial depth alone does not specify the amount.

Worked porosity example: compaction and cement

Also called: Physical compaction

References & related terms

AAPG Development Geology Reference Manual — Reservoir quality (Grier and Marschall) Reference checked 2026-10-27

Additional interpretation reference

Related: Pressure solution · Compaction · Diagenesis

View schematic: Mechanical packing and pressure solution

Reservoir geology#

Pressure solution

Stress-assisted dissolution at mineral contacts, coupled to transport of dissolved material through a fluid. Removal of material from loaded contacts permits grains to approach and the framework to shorten. Dissolved material may precipitate elsewhere or leave the local rock volume.

Field context Look for truncated or sutured contacts and dissolution seams in their petrographic context. A dark seam alone does not prove pressure solution, quantify shortening, or identify where dissolved material was deposited. Record serrated contacts, residue and any later opening separately. The conceptual guide distinguishes dissolution evidence from a visible gap; neither alone supplies a measured permeability.

Worked observations: stylolite seam versus open fracture

Also called: Pressure dissolution

References & related terms

AAPG Development Geology Reference Manual — Reservoir quality (Grier and Marschall) Reference checked 2026-10-27

Field-context reference

Additional interpretation reference

Related: Mechanical compaction · Compaction · Diagenesis

Additional schematic: Stylolite seam versus open fracture

View schematic: Mechanical packing and pressure solution

Hydrogeology & pore systems#

Hydraulic diffusivity

Ratio of an aquifer’s ability to transmit water to its capacity to release water from storage as head changes. For a homogeneous confined system, D = T/S = K/Ss, with area-per-time units. It controls the rate of hydraulic-head redistribution in the corresponding diffusion model; it is not a pore-water velocity.

Field context State geometry, storage mechanism and boundary conditions. A timescale based on distance squared divided by D is not a contaminant travel time, a sharp pressure front or a universal pumping-test duration. Equal diffusivity fixes the same Theis response coordinate at equal distance and time, but drawdown also depends on Q/T. Doubling both T and S at fixed pumping rate leaves diffusivity unchanged while halving ideal Theis drawdown.

Worked example: equal diffusivity, different drawdown

Also called: Aquifer diffusivity

References & related terms

Herbert F. Wang (2020), The Groundwater Project — Diffusion Equation Reference checked 2026-10-31

Additional interpretation reference

Related: Transmissivity · Storativity · Specific storage · Potentiometric surface

View schematic: Confined head response and hydraulic diffusivity

Hydrogeology & pore systems#

Potentiometric surface

A surface representing hydraulic-head elevations in a specified aquifer, inferred from water levels in wells or piezometers hydraulically connected to that unit. In a confined aquifer it can lie above the aquifer roof without being a boundary between saturated and unsaturated rock.

Field context Identify the connected interval, measurement time, elevation datum and fluid-density convention. Mixing screens from different units or dates can create a misleading surface; vertical head gradients may require separate depth-specific representations. Compare head with outlet elevation when distinguishing non-flowing from flowing artesian conditions.

Worked hydraulic response and head interpretation

Also called: Piezometric surface

References & related terms

Cohen and Cherry (2020), The Groundwater Project — Hydraulics of Flow in Confined Aquifers Reference checked 2026-10-29

Field-context reference

Additional interpretation reference

Related: Hydraulic head · Hydraulic diffusivity · Storativity · Artesian condition · Confined aquifer

View schematic: Confined head response and hydraulic diffusivity

Reservoir geology#

Flexural slip

Folding accommodated in part by relative movement on discrete surfaces approximately parallel to layering. Slip between beds or rock packets permits them to rotate while limiting deformation within each packet; natural folds may also undergo internal strain.

Field context Look for displaced cross-cutting markers, movement surfaces and consistent shear-sense evidence. Bedding-parallel veins alone do not measure slip, and a parallel fold shape does not uniquely establish this mechanism.

Worked folding geometry and slip evidence

Also called: Flexural-slip folding

References & related terms

University of Michigan, Processes in Structural Geology and Tectonics — Folds Reference checked 2026-10-27

Additional interpretation reference

Related: Fold · Bedding · Flexural flow

View schematic: Folding: localized slip, distributed shear and arc lengths

Reservoir geology#

Flexural flow

Folding accommodated by layer-parallel shear distributed within rock layers at a finer scale than discrete interbed slip surfaces. It is a kinematic description of how deformation is spread through a layered rock, rather than evidence that the rock melted.

Field context Distinguish distributed strain from localized flexural slip using internal markers and fabrics. Both can contribute to one fold; a model result for a specified layering and rheology is not a universal dip threshold for slip onset.

Worked folding geometry and slip evidence

Also called: Flexural-flow folding

References & related terms

University of Michigan, Processes in Structural Geology and Tectonics — Folds Reference checked 2026-10-27

Additional interpretation reference

Related: Fold · Bedding · Flexural slip

View schematic: Folding: localized slip, distributed shear and arc lengths

Reservoir geology#

Walther’s law

In a conformable depositional succession, vertically adjoining facies can represent environments that were laterally adjacent as those environments migrated. The principle links spatial relationships to vertical stacking; it does not make matching rock types the same age.

Field context Test continuity and environmental interpretation before applying the principle. Erosion, nondeposition, structural repetition and missing core can interrupt the apparent succession.

Worked example: migrating facies and a missing interval

Also called: Walther's law of facies, Law of facies succession

References & related terms

Dawn Sumner, UC Davis — Sediments and Strata Reference checked 2026-10-27

Additional interpretation reference

Related: Facies · Facies association · Progradation · Diachronous

View schematic: Facies migration: time slices and a preserved vertical record

Reservoir geology#

Facies association

A group of facies interpreted as genetically or environmentally related from their characteristics and spatial arrangement. An association combines evidence from several facies to help reconstruct a depositional setting; its grouping criteria should be stated.

Field context Keep observed textures, structures and fossils distinct from the interpreted environment. Association labels such as FA1 are local codes, not universal stratigraphic units or time markers.

Worked example: migrating facies and a missing interval

Also called: Sedimentary facies association

References & related terms

Dawn Sumner, UC Davis — Sedimentary Facies Reference checked 2026-10-27

Related: Facies · Depositional environment · Walther’s law

View schematic: Facies migration: time slices and a preserved vertical record

Reservoir geology#

Baselap

A general term for stratal terminations against a lower bounding surface, encompassing onlap and downlap. It is useful when their distinction cannot be resolved, for example after deformation obscures the original geometry.

Field context Record which side of the surface contains the terminating package. Preserve the uncertainty rather than assigning a depositional direction from the present apparent dip alone.

Worked interpretation: reflection terminations and uncertainty

Also called: Basal lap

References & related terms

SEPM STRATA — Seismic Interpretation Reference checked 2026-10-28

Related: Onlap · Downlap · Toplap · Sequence stratigraphy

View schematic: Reflection terminations: identify the bounding surface first

Reservoir geology#

Toplap

Termination of strata beneath an overlying surface, interpreted mainly as nondeposition or sediment bypass, with possible minor erosion. It differs from substantial erosional removal that truncates previously deposited strata.

Field context A contact sketch alone does not establish how much sediment was removed. Distinguish the observed upper termination from the proposed process and seek supporting stratigraphic evidence.

Worked interpretation: reflection terminations and uncertainty

Also called: Top lap

References & related terms

SEPM STRATA — Toplap Reference checked 2026-10-28

Additional interpretation reference

Related: Onlap · Downlap · Baselap · Unconformity

View schematic: Reflection terminations: identify the bounding surface first

Logging & geology#

Isograd

A mapped line marking a specified change in metamorphic mineral occurrence or assemblage, commonly the first appearance of an index mineral toward higher grade in rocks of suitable composition. In three dimensions the boundary is a surface.

Field context Specify the mineral-in, mineral-out or reaction criterion. A change of protolith chemistry, incomplete reaction or later overprint can mimic or obscure the boundary; a mineral occurrence alone is not a temperature measurement.

Worked guide: mineral evidence, isograds and overprints

Also called: Metamorphic isograd

References & related terms

Tulane University — Metamorphic Reactions, Isograds, and Reaction Mechanisms Reference checked 2026-10-28

Related: Retrograde metamorphism · Chlorite · Mineral replacement · Mineral assemblage · Metamorphic dehydration reaction

View schematic: Isograd evidence and a later mineral overprint

Logging & geology#

Retrograde metamorphism

Metamorphic mineral or textural change that overprints an earlier higher-temperature assemblage under lower-temperature conditions, commonly during cooling and exhumation. Reactions may be incomplete, leaving older minerals beside later products.

Field context Fluid access and reaction rates affect preservation. Establish the sequence from textures and mineral associations; chlorite alone does not prove a retrograde history. Distinguish this process from sedimentary retrogradation and hydrocarbon retrograde condensation.

Worked guide: mineral evidence, isograds and overprints

Also called: Metamorphic retrogression

References & related terms

Tulane University — Metamorphic Mineral Assemblages Reference checked 2026-10-28

Related: Isograd · Chlorite · Mineral replacement · Mineral assemblage · Metamorphic dehydration reaction

View schematic: Isograd evidence and a later mineral overprint

Reservoir engineering#

Capillary-pressure hysteresis

Dependence of capillary pressure on the path by which a porous material reached its present fluid saturation. Drainage and subsequent imbibition can give different pressure differences at the same saturation.

Field context State the wetting phase, pressure sign and reversal history. A single saturation value does not identify a unique pressure difference; hysteresis is not simply measurement error.

Worked example: saturation and displacement history

Also called: Capillary hysteresis

References & related terms

Idaho National Laboratory MOOSE — Hysteresis in PorousFlow Reference checked 2026-10-28

Related: Capillary pressure · Wettability · Drainage displacement · Imbibition

View schematic: Same saturation, different displacement history

Wellsite geology & samples#

Solvus

An equilibrium phase boundary marking the compositional limit of a solid solution at specified conditions. In a binary temperature–composition diagram at fixed pressure, a solvus can bound a region where two solid phases coexist instead of one homogeneous solid solution.

Field context A solvus is a stability boundary, not a melting boundary or a clock. A natural mineral may preserve disequilibrium textures, and an actual phase diagram must match its chemical system and pressure.

Worked example: composition and phase abundance

Also called: Solid-solubility boundary

References & related terms

Tulane University — Two Component (Binary) Phase Diagrams Reference checked 2026-10-28

Related: Lever rule · Mineral exsolution · Perthite

View schematic: Composition is not phase abundance

Wellsite geology & samples#

Lever rule

A two-phase balance that calculates the proportions of coexisting phases from their compositions and the bulk composition. On a binary diagram, a phase fraction equals the tie-line segment from the bulk composition to the opposite phase, divided by the complete tie-line length.

Field context Use one consistent composition basis: mass-fraction coordinates give mass fractions, not volume fractions. Equilibrium phase-boundary endpoints are valid only for the specified conditions; an observed texture alone does not supply them.

Worked example: composition and phase abundance

Also called: Phase-proportion lever rule

References & related terms

University of Southampton — Tie Lines and the Lever Rule Reference checked 2026-10-28

Related: Solvus · Mineral exsolution · Perthite

View schematic: Composition is not phase abundance

Reservoir geology#

Taxon-range zone

A biostratigraphic unit encompassing the documented stratigraphic and geographic occurrences of one taxon. In an individual section, its local limits are the lowest and highest accepted occurrences of that taxon.

Field context Specify the section and taxonomic identification. A local range need not span the entire known distribution of the taxon.

Worked example: fossil ranges and sample uncertainty

Also called: Taxon-range biozone

References & related terms

International Commission on Stratigraphy — Stratigraphic Guide, Biostratigraphic Units Reference checked 2026-10-28

Related: Concurrent-range zone · Biostratigraphy · Palynology · Reworked fossil · Biohorizon · Interval biozone

View schematic: Observed fossil ranges and their overlap

Reservoir geology#

Concurrent-range zone

A biostratigraphic unit defined by the overlapping ranges of two specified taxa. In a section, its base is the higher of their lowest occurrences and its top is the lower of their highest occurrences.

Field context Two taxa define this overlap; other fossils may also occur. The zone is a body of strata, not automatically a globally synchronous time interval.

Worked example: fossil ranges and sample uncertainty

Also called: Concurrent-range biozone

References & related terms

North American Commission on Stratigraphic Nomenclature — Code, Articles 49–51 Reference checked 2026-10-28

Related: Taxon-range zone · Biostratigraphy · Palynology · Reworked fossil · Biohorizon · Interval biozone

View schematic: Observed fossil ranges and their overlap

Reservoir geology#

Isotope delta

Relative difference between a specified isotope ratio in a sample and the same ratio in a reference: δ = Rsample/Rreference − 1. It is dimensionless; a value of −0.010 is commonly written −10 ‰. State the isotope pair and reference scale.

Field context A negative delta means a lower heavy-to-light isotope ratio than the reference, not a negative isotope abundance. Delta is neither an element concentration nor, by itself, a geological age. Changing the reference ratio changes delta even when the sample is unchanged. Convert through ratios and retain the documented scale relationship; subtracting a constant delta offset is not generally exact.

Worked example: one sample, two hypothetical references

Also called: Stable-isotope delta notation, Relative isotope-ratio difference

References & related terms

Coplen (2011) — Guidelines for stable-isotope-ratio measurement results Reference checked 2026-10-28

Related: Isotope fractionation · Radiogenic isotope · Diagenesis

View schematic: Isotope delta: compare ratios on the same reference scale

Reservoir geology#

Isotope fractionation

Redistribution of isotopes of an element between materials during physical, chemical or biological processes. Equilibrium partitioning and differences in reaction or transport rates can produce different isotope ratios; the mechanism needs independent evidence.

Field context For the same isotope pair, αA/B = RA/RB describes a specified pair of materials. Identify their order and whether the value describes equilibrium, a kinetic process or only an observed distribution; a ratio contrast alone does not establish the cause. A delta-value difference is not exactly 1000(α − 1): for −10‰ and −20‰ on one scale, these are 10‰ and about 10.204‰ respectively.

Stable isotopes: delta values, ratios and interpretation

Also called: Isotopic fractionation

References & related terms

Kendall and Caldwell (1998) — Fundamentals of Isotope Geochemistry, sections 2.2–2.3 Reference checked 2026-10-30

Field-context reference

Additional interpretation reference

Related: Isotope delta · Diagenesis · Radiogenic isotope

View schematic: Isotope delta: compare ratios on the same reference scale

Reservoir geology#

Partial melting

Formation of melt from only part of a rock, leaving a solid residue. Melt and residue commonly differ in composition; their proportions and chemistry depend on the source, conditions and whether melt remains in contact with the solid or is extracted.

Field context A melt fraction is a proportion, not a temperature. Distinguish the source rock, residual solid and extracted melt; do not treat a mixed whole-rock analysis as the composition of each phase.

Worked example: melting versus crystal removal

Also called: Incomplete melting

References & related terms

Stephen A. Nelson / Tulane University — Magmatic Differentiation Reference checked 2026-10-28

Additional interpretation reference

Related: Fractional crystallization · Mineral–melt partition coefficient · Incompatible element

View schematic: Melting and crystal removal: two separate mass balances

Reservoir geology#

Fractional crystallization

Igneous differentiation in which growing crystals become separated from effective chemical exchange with the remaining melt. Removing a mineral assemblage changes the residual liquid according to the composition and amount of material isolated.

Field context Physical settling is one possible mechanism, not a requirement. Distinguish crystal removal from partial melting, isotope fractionation and petroleum product separation. An accumulated crystal composition is not an instantaneous equilibrium partition coefficient.

Worked example: melting versus crystal removal

Also called: Crystal fractionation, Fractional crystallisation

References & related terms

Stephen A. Nelson / Tulane University — Magmatic Differentiation Reference checked 2026-10-28

Additional interpretation reference

Related: Partial melting · Mineral–melt partition coefficient · Compatible element

View schematic: Melting and crystal removal: two separate mass balances

Reservoir geology#

Paleosol

A soil formed on a landscape of the past. It may survive beneath younger deposits, be exposed again after burial, or remain at the surface as a relict of former conditions.

Field context Colour alone does not establish a paleosol. Evaluate profile organization, root traces, soil structure and alteration; burial is not required by the broad definition.

Worked example: test a buried-soil interpretation

Also called: Palaeosol, Ancient soil

References & related terms

USGS — Soils and paleosols Reference checked 2026-10-28

Related: Soil horizon

View schematic: Buried soil versus a coloured sedimentary bed

Reservoir geology#

Soil horizon

A layer within a soil profile distinguished from adjacent layers by properties developed or modified during soil formation, such as structure, texture, organic matter or chemistry.

Field context A soil horizon is not automatically a sedimentary bed or an equal-time surface. Record the classification system and observed properties; not every profile contains all master horizons.

Worked example: test a buried-soil interpretation

Also called: Pedologic horizon

References & related terms

USDA NRCS — A Soil Profile Reference checked 2026-10-28

Related: Paleosol

View schematic: Buried soil versus a coloured sedimentary bed

Hydrogeology & pore systems#

Aquitard

A geological unit that restricts groundwater transmission relative to adjacent aquifers but can still pass water. It may store water while yielding too little, too slowly, to function as a productive aquifer.

Field context Aquitard describes hydraulic behaviour, not a rock name. Fractures and discontinuities can change effective confinement; a shale label alone does not demonstrate hydraulic isolation.

Worked example: aquitard leakage and head reversal

Also called: Leaky confining bed

References & related terms

US Bureau of Reclamation — Engineering Geology Field Manual, Chapter 9, definitions Reference checked 2026-10-28

Related: Aquifer · Vertical leakance · Hydraulic conductivity

View schematic: Head-driven leakage across an aquitard

Hydrogeology & pore systems#

Vertical leakance

Vertical hydraulic conductivity divided by the thickness of a confining layer: L = Kv/b, with units of inverse time. For steady one-dimensional flow, multiplying L by the head difference across that layer gives the vertical Darcy flux.

Field context Leakance is not flux or volumetric flow rate. For a uniform area A, conductance is A × L and total flow is A × L × head difference. State the thickness, fluid and hydraulic model; transient storage and bypass paths can invalidate this simple estimate.

Worked example: aquitard leakage and head reversal

Also called: Leakance coefficient

References & related terms

The Groundwater Project — Hantush–Jacob solution, vertical leakance Reference checked 2026-10-28

Related: Aquitard · Hydraulic head · Darcy flux · Hydraulic conductivity

View schematic: Head-driven leakage across an aquitard

Reservoir geology#

Fissility

The tendency of a rock to separate into thin, closely spaced sheets. In shale, this splitting commonly follows sedimentary bedding; the property describes breakage and is not synonymous with visible lamination.

Field context Describe the split surfaces and their relationship to layering. Tectonic cleavage can also produce thin plates, so a flat chip alone does not establish sedimentary fissility, geographic dip or a quantified rock strength.

Worked comparison: splitting versus layering

Also called: Fissile splitting, Shaly fissility

References & related terms

Arkansas Geological Survey — Shale Reference checked 2026-10-28

Additional interpretation reference

Related: Shale · Mudstone · Lamination · Rock cleavage

View schematic: Fissility, lamination and tectonic cleavage

Reservoir geology#

Aragonite

A calcium carbonate mineral, CaCO3, with an orthorhombic crystal structure. It is a polymorph of calcite and occurs in many biological hard parts as well as inorganic mineral deposits.

Field context A chemical formula alone does not distinguish polymorphs. Record current mineral identification separately from external shape and any proposed precursor; inherited form does not demonstrate present crystal structure.

Worked identification: composition versus crystal structure

Also called: Aragonitic calcium carbonate

References & related terms

Tulane University — Twinning, Polymorphism, Polytypism, Pseudomorphism Reference checked 2026-10-28

Additional interpretation reference

Related: Calcite · Polymorphism · Pseudomorph · Mineral replacement

View schematic: Same composition, different mineral structures

Reservoir geology#

Polymorphism

The occurrence of the same chemical composition in two or more different crystal structures; calcite and aragonite are calcium carbonate examples.

Field context A chemical formula alone does not distinguish polymorphs. Record current mineral identification separately from external shape and any proposed precursor; inherited form does not demonstrate present crystal structure.

Worked identification: composition versus crystal structure

Also called: Mineral polymorphism

References & related terms

Tulane University — Twinning, Polymorphism, Polytypism, Pseudomorphism Reference checked 2026-10-28

Additional interpretation reference

Related: Calcite · Aragonite · Pseudomorph · Mineral replacement

View schematic: Same composition, different mineral structures

Reservoir geology#

Stylolite

An irregular, interlocking dissolution surface with tooth-like relief, commonly outlined by residue less soluble than the surrounding rock. It records localized pressure solution rather than simply an open crack.

Field context Record serrated contacts, residue and any later opening separately. The conceptual guide distinguishes dissolution evidence from a visible gap; neither alone supplies a measured permeability.

Worked observations: stylolite seam versus open fracture

Also called: Stylolitic seam

References & related terms

SLB Energy Glossary — stylolite Reference checked 2026-10-28

Related: Pressure solution · Diagenesis

Additional schematic: Stylolite seam versus open fracture

View schematic: Stylolite seam versus open fracture

Reservoir geology#

Streak

The colour of a mineral powder, used as one observation in mineral identification. It may differ from the colour of the intact grain.

Field context Distinguish mineral powder from a groove or debris produced by scratching the porcelain itself. A failed plate test leaves streak unassessed, not necessarily white. Scratch tests compare resistance to scratching; a chip breaking during a test is not a hardness measurement. Record the reference material and confirm a groove rather than loose powder.

Worked example: streak powder or scratched plate?

Also called: Mineral streak

References & related terms

Mineralogical Society of America — Mineral Identification Key: Streak Reference checked 2026-10-28

Related: Streak plate · Mineral cleavage

View schematic: Streak powder or scratched plate?

Reservoir geology#

Streak plate

An unglazed porcelain test surface used to produce and examine a mineral powder streak. Minerals harder than the plate may scratch it instead.

Field context A typical porcelain plate is about Mohs 6.5, so harder minerals may scratch the plate instead of yielding a useful powder streak. Treat the plate as a test material with limitations, not a universal colour detector.

Worked example: streak powder or scratched plate?

References & related terms

Mineralogical Society of America — Mineral Identification Key: Streak Reference checked 2026-10-28

Related: Streak · Mineral cleavage

View schematic: Streak powder or scratched plate?

Reservoir geology#

Net pay

Summed thickness of intervals interpreted to satisfy stated reservoir-quality and hydrocarbon criteria for potential production within a defined gross interval. The cutoffs and evaluation purpose must be specified; an interpreted net-pay flag alone does not establish commercial viability.

Worked example: specify which net-to-gross ratio

Also called: Net pay thickness

References & related terms

SLB Energy Glossary — pay Reference checked 2026-10-28

Related: Net-to-gross ratio · Porosity · Permeability

View schematic: Qualifying a net-to-gross ratio

Reservoir geology#

Net-to-gross ratio NTG

Dimensionless ratio of selected net thickness to the corresponding gross interval thickness, using consistent boundaries and measurement direction. Qualify the numerator, such as net reservoir or net pay, and report the selection criteria; these ratios are not interchangeable.

Worked example: specify which net-to-gross ratio

Also called: Net to gross ratio, Net/gross ratio

References & related terms

Worthington (2010), Net Pay — SPE Reservoir Evaluation & Engineering; publisher summary Reference checked 2026-10-28

Additional interpretation reference

Related: Net pay · True stratigraphic thickness · True vertical thickness · Isopach · Isochore

View schematic: Qualifying a net-to-gross ratio

Reservoir geology#

Marine flooding surface

A stratigraphic contact interpreted to record an abrupt shift to deeper-water deposition above shallower-water deposits. The interpretation rests on facies evidence across the contact; the surface can include minor submarine erosion. Such surfaces commonly bound parasequences.

Field context Keep the observed contact separate from the inferred water-depth change. A mud-over-sand contact alone is insufficient, and an ordinary flooding surface is not automatically a maximum flooding surface.

Worked example: flooding surfaces and parasequence evidence

Also called: Flooding surface

References & related terms

SLB Energy Glossary — flooding surface Reference checked 2026-10-28

Additional interpretation reference

Related: Parasequence · Maximum flooding surface · Facies

View schematic: Parasequence boundaries and evidence

Wellsite geology & samples#

Mineral tenacity

A description of how a mineral responds to breaking or deformation, including bending, crushing or cutting. Tenacity concerns mechanical behaviour, whereas mineral hardness describes resistance to scratching.

Field context In mineral-identification usage, flexible material stays bent after release; elastic material recovers its earlier shape. Report the observed specimen behaviour without inferring a numerical strength or a unique mineral identity.

Worked example: bending, recovery and scratch hardness

Also called: Tenacity (mineralogy), Tenacity

References & related terms

Mineralogical Society of America — Mineral ID Key: Tenacity Reference checked 2026-10-29

Additional interpretation reference

Related: Mineral cleavage · Mineral fracture

View schematic: Flexible versus elastic mineral behaviour

Hydrogeology & pore systems#

Artesian condition

Confined groundwater pressure that raises water above the aquifer top in a well; surface flow is not required.

Field context Compare static head with both the aquifer roof and the discharge outlet using the same elevation datum. A level above the roof can remain below land. Head above an outlet indicates discharge potential, but does not determine flow rate.

Worked example: artesian head and surface flow

Also called: Artesian pressure

References & related terms

USGS Water Science School — Water Science Glossary Reference checked 2026-10-29

Additional interpretation reference

Related: Aquifer · Water table · Confined aquifer · Potentiometric surface

View schematic: Artesian head versus outlet elevation

Hydrogeology & pore systems#

Confined aquifer

Aquifer beneath a confining layer, with water pressure sufficient to raise a well water level above its top.

Field context Compare static head with both the aquifer roof and the discharge outlet using the same elevation datum. A level above the roof can remain below land. Head above an outlet indicates discharge potential, but does not determine flow rate.

Worked example: artesian head and surface flow

References & related terms

USGS Water Science School — Water Science Glossary Reference checked 2026-10-29

Additional interpretation reference

Related: Aquifer · Water table · Artesian condition · Potentiometric surface

View schematic: Artesian head versus outlet elevation

Reservoir geology#

Pyroxene

A group of silicate minerals with single-chain structures, commonly present in mafic igneous rocks.

Field context Two cleavage directions near a right angle can support a pyroxene identification in a suitable section; they do not identify an end-member composition.

Worked example: pyroxene composition

References & related terms

Steven Earle / BCcampus — Physical Geology: Silicate Minerals Reference checked 2026-10-29

Additional interpretation reference

Related: Ophitic texture

View schematic: Diopside and hedenbergite: ideal end-member chemistry

Reservoir geology#

Hummocky cross-stratification HCS

Low-angle cross-stratification with gently curved convex-up and concave-up laminae, variable dip directions and local truncation surfaces. Commonly associated with storm-influenced deposition.

Field context Describe geometry and sample orientation before assigning process; a small chip cannot establish the full architecture of a bed.

Worked example: reversing flow with a mean current

Also called: Hummocky cross-bedding

References & related terms

Dumas & Arnott (2006), Geology — Hummocky and swaley cross-stratification Reference checked 2026-10-29

Related: Wave ripple · Cross-bedding · Combined flow

View schematic: Combined flow: reversal with a mean current

Reservoir geology#

Combined flow

Flow containing both oscillatory motion and a unidirectional current component. Their relative strength and orientation influence near-bed motion and sedimentary bedforms.

Field context Describe geometry and sample orientation before assigning process; a small chip cannot establish the full architecture of a bed.

Worked example: reversing flow with a mean current

Also called: Wave–current combined flow

References & related terms

Dumas, Arnott & Southard (2005), AAPG conference abstract Reference checked 2026-10-29

Related: Wave ripple · Cross-bedding · Hummocky cross-stratification

View schematic: Combined flow: reversal with a mean current

Hydrogeology & pore systems#

Piezometer

A device measuring fluid pressure at a selected location or isolated interval. In an open standpipe containing water of uniform density, the stabilized water-level elevation represents hydraulic head at the connected measurement point.

Field context State the elevation sign convention and measurement interval. Long screens can combine responses from multiple elevations; their midpoint is an approximation, not a point measurement.

Worked example: higher head at a deeper measurement point

Also called: Standpipe piezometer

References & related terms

Cohen and Cherry — Darcian head profiles Reference checked 2026-10-29

Field-context reference

Related: Hydraulic head · Hydraulic gradient · Vertical hydraulic gradient

View schematic: Vertical gradient: screen elevation versus head

Hydrogeology & pore systems#

Vertical hydraulic gradient

Change in hydraulic head per unit vertical distance. With elevation z positive upward, dh/dz is signed; under one-dimensional constant-density Darcy flow, qz = −Kz dh/dz.

Field context State the elevation sign convention and measurement interval. Long screens can combine responses from multiple elevations; their midpoint is an approximation, not a point measurement.

Worked example: higher head at a deeper measurement point

Also called: Vertical head gradient

References & related terms

Cohen and Cherry — Darcian head profiles Reference checked 2026-10-29

Field-context reference

Related: Hydraulic head · Hydraulic gradient · Piezometer · Gaining stream · Losing stream

View schematic: Vertical gradient: screen elevation versus head

Reservoir geology#

Fossil mould

A natural impression of a fossil surface in its surrounding material. State whether the impression represents an exterior or an interior surface.

Field context Specify the surface represented: an external mould records the outside of a shell. In a broken cutting, record the visible impression before inferring a complete organism.

Worked example: describe a mould, cast or steinkern

Also called: Fossil mold

References & related terms

National Park Service — Mold, Casts, and Steinkerns Reference checked 2026-10-29

Related: Fossil · Moldic porosity · Fossil cast

View schematic: Mould, cast or steinkern: which surface survives?

Reservoir geology#

Fossil cast

A solid replica formed by filling a natural fossil mould with sediment or mineral material.

Field context A cast is infill, not surviving shell material. Record the fill and surrounding rock separately; do not equate a filled fossil shape with an open pore.

Worked example: describe a mould, cast or steinkern

References & related terms

National Park Service — Mold, Casts, and Steinkerns Reference checked 2026-10-29

Related: Fossil · Moldic porosity · Fossil mould

View schematic: Mould, cast or steinkern: which surface survives?

Reservoir geology#

Weathering

Physical disintegration or chemical alteration of rock at or near the Earth’s surface, before transport by erosion.

Field context Breakage can increase exposed surface without changing solid volume. Keep observations of coatings and altered surfaces separate from fresh interiors; smaller fragments alone do not establish a chemical reaction rate.

Worked example: breakage and exposed surface area

References & related terms

Salt Lake Community College — Weathering, Erosion, and Sedimentary Rocks Reference checked 2026-10-29

Related: Mineral (Geology Dictionary) · Grain size

View schematic: Breakage exposes more surface

Reservoir geology#

Biohorizon

A surface marking a significant change in fossil content or distribution within a stratigraphic succession. It has no thickness; it is not a name for a thin fossil-rich bed.

Field context Record the fossil criterion and sampling resolution. An observed local occurrence limit does not by itself establish a global evolutionary event.

Worked example: interval boundaries without range overlap

Also called: Biostratigraphic horizon

References & related terms

International Commission on Stratigraphy — Guide, chapter 7, section C.4 Reference checked 2026-10-30

Related: Interval biozone · Taxon-range zone · Biostratigraphy

View schematic: Interval boundaries without overlapping fossil ranges

Reservoir geology#

Interval biozone

A biostratigraphic unit bounded by two specified fossil-based surfaces. Its defining taxa need not coexist or extend through the full interval.

Field context State whether each boundary uses a lowest occurrence, highest occurrence or another specified feature. In cuttings, document drilling direction and possible contamination before picking a boundary.

Worked example: interval boundaries without range overlap

Also called: Interval zone

References & related terms

North American Stratigraphic Code — Articles 50–51 Reference checked 2026-10-30

Related: Biohorizon · Concurrent-range zone · Biostratigraphy · Cavings · Assemblage biozone · Abundance biozone · Lineage biozone

View schematic: Interval boundaries without overlapping fossil ranges

Hydrogeology & pore systems#

Kinematic viscosity

Dynamic viscosity divided by fluid density: ν = μ/ρ. Its SI unit is square metres per second. It describes viscous momentum diffusion and differs from dynamic viscosity, whose SI unit is pascal-second.

Field context Use density and viscosity at the same stated conditions. In the saturated, single-phase Darcy relation K = kρg/μ, substitution gives K = kg/ν. Neither viscosity nor conductivity alone is the pore-water travel speed.

Worked example: dynamic versus kinematic viscosity

Also called: Momentum diffusivity

References & related terms

NASA Glenn Research Center — Viscosity Reference checked 2026-10-30

Related: Hydraulic conductivity · Permeability

View schematic: Same pore network, different hydraulic conductivity

Hydrogeology & pore systems#

Molecular diffusion

Redistribution of dissolved species by molecular motion, producing net transport down a concentration gradient in a simple Fickian description. It can occur without bulk water flow. A diffusion coefficient has dimensions of length squared per time; its value depends on the species, temperature and medium.

Field context Distinguish free-water diffusion from a porous-medium effective coefficient. Report whether porosity is included in the coefficient or applied separately to flux; conventions differ between transport models. Diffusion is distinct from mechanical dispersion and hydraulic pressure diffusion.

Worked example: molecular diffusion with no mean water flow

Also called: Molecular solute diffusion

References & related terms

Penn State CE 574 — 6.3 Diffusion Reference checked 2026-10-30

Related: Mechanical dispersion · Dispersivity · Average linear groundwater velocity · Hydraulic diffusivity

View schematic: Solute movement and spreading are different quantities

Logging & geology#

Mineral assemblage

A group of minerals occurring together in a rock or a specified part of it. An equilibrium assemblage is the more restrictive interpretation that those phases coexisted in chemical equilibrium under the conditions being considered.

Field context A whole-sample mineral list can mix inclusions, relict grains and later replacement products. State the observed domain and texture before treating every listed mineral as a single equilibrium group.

Worked example: dehydration and reaction progress

Also called: Mineral association

References & related terms

Tulane University — Metamorphic Mineral Assemblages Reference checked 2026-10-30

Related: Metamorphic dehydration reaction · Isograd · Retrograde metamorphism

View schematic: Metamorphic dehydration: balance and reaction progress

Logging & geology#

Metamorphic dehydration reaction

A mineral reaction that releases H₂O from structurally bound hydrogen and oxygen in hydrous minerals into a fluid phase. It changes the solid mineral assemblage and differs from drainage or evaporation of pre-existing pore water.

Field context Water production does not establish that fluid escaped the rock. The balanced reaction specifies material accounting, while pressure, temperature, fluid composition and reaction progress require separate evidence.

Worked example: dehydration and reaction progress

Also called: Dehydration reaction (metamorphism)

References & related terms

Tulane University — Metamorphic Reactions, Isograds, and Reaction Mechanisms Reference checked 2026-10-30

Related: Mineral assemblage · Isograd · Retrograde metamorphism

View schematic: Metamorphic dehydration: balance and reaction progress

Logging & geology#

Gaining stream

A stream reach receiving groundwater discharge through its bed or banks. The designation describes the exchange direction for a specified reach and time.

Field context A gaining reach can become losing as relative heads change; record the observation date and reach extent.

Worked example: streambed head reversal

Also called: Effluent stream

References & related terms

USGS Circular 1139 — Ground Water and Surface Water: A Single Resource Reference checked 2026-10-30

Additional interpretation reference

Related: Losing stream · Hydraulic head · Water table · Vertical hydraulic gradient

View schematic: Streambed seepage and head reversal

Logging & geology#

Losing stream

A stream reach supplying water to the subsurface through its bed or banks. It can remain connected to groundwater through saturated sediment or be separated from the water table by an unsaturated zone.

Field context Losing describes exchange direction, not whether a stream is perennial. Check hydraulic connection before applying a saturated streambed-flow calculation.

Worked example: streambed head reversal

Also called: Influent stream

References & related terms

USGS Circular 1139 — Ground Water and Surface Water: A Single Resource Reference checked 2026-10-30

Additional interpretation reference

Related: Gaining stream · Hydraulic head · Water table · Vertical hydraulic gradient

View schematic: Streambed seepage and head reversal

Reservoir geology#

Median grain size

Particle diameter at the 50th percentile of a specified grain-size distribution. For a cumulative percent-finer curve weighted by mass, it divides the represented sample mass into finer and coarser halves; the weighting and measurement method are part of the reported result.

Field context A median is not generally the arithmetic or geometric mean. A sieve bracket can constrain D50 without measuring it exactly; interpolation requires an explicitly chosen coordinate. Washed cuttings may exclude formation fines, so qualify the population represented.

Worked example: median size from sieve fractions

Also called: D50, Median particle size

References & related terms

FHWA-RD-03-083 — sediment mixtures and grain-size distributions Reference checked 2026-10-30

Additional interpretation reference

Related: Grain size · Sorting · Phi scale · Sieve analysis

View schematic: Reading D50 from cumulative sieve masses

Reservoir geology#

Sieve analysis

Laboratory particle-size analysis that separates a prepared granular sample using mesh openings of known dimensions and measures the material retained in successive fractions. Reporting retained masses and cumulative percent passing describes a size distribution for the tested sample.

Field context Report aperture dimensions, preparation, mass recovery and the treatment of material finer than the smallest sieve. Sieving cemented drill chips measures chip sizes unless the original grains have been liberated; a molecular sieve is an adsorbent, not this sediment test.

Worked example: median size from sieve fractions

Also called: Sieve-size analysis

References & related terms

USGS Thesaurus — sieve-size analysis Reference checked 2026-10-30

Additional interpretation reference

Related: Grain size · Median grain size · Sorting

View schematic: Reading D50 from cumulative sieve masses

Reservoir geology#

Poikilitic texture

A crystal-enclosure texture in which a larger host crystal contains numerous smaller crystals of one or more other minerals. The host is termed an oikocryst and the enclosed crystals chadacrysts; the name describes their relationship rather than a particular mineral pair.

Field context Describe the observed section and distinguish host continuity from similar colour. A broken cutting may truncate a crystal boundary, and a two-dimensional view cannot establish every three-dimensional connection. This texture alone does not specify a cooling rate, magma source or permeability. Describe grain size relative to the surrounding groundmass separately from crystal enclosure. A phenocryst need not contain smaller crystals, and a poikilitic host need not be a phenocryst. Size contrast alone does not identify a unique cooling history.

Worked comparison: grain size versus enclosure

Also called: Poikilitic

References & related terms

IODP Expedition 402 — Methods, igneous grain relationships Reference checked 2026-10-30

Additional interpretation reference

Related: Ophitic texture · Subophitic texture · Plagioclase (Geology Dictionary) · Pyroxene · Porphyritic texture (Geology Dictionary)

View schematic: Crystal enclosure: poikilitic, ophitic and subophitic

Reservoir geology#

Ophitic texture

A poikilitic relationship in which plagioclase laths are wholly enclosed by larger pyroxene crystals, commonly clinopyroxene. It is characteristic of some mafic igneous rocks but is a texture, not a rock name.

Field context Describe the observed section and distinguish host continuity from similar colour. A broken cutting may truncate a crystal boundary, and a two-dimensional view cannot establish every three-dimensional connection. This texture alone does not specify a cooling rate, magma source or permeability.

Worked example: crystal enclosure versus grain size

Also called: Ophitic

References & related terms

IODP Expedition 402 — Methods, igneous grain relationships Reference checked 2026-10-30

Additional interpretation reference

Related: Poikilitic texture · Subophitic texture · Plagioclase (Geology Dictionary) · Pyroxene · Porphyritic texture (Geology Dictionary)

View schematic: Crystal enclosure: poikilitic, ophitic and subophitic

Reservoir geology#

Subophitic texture

An igneous grain relationship in which pyroxene only partly encloses plagioclase laths. In the convention used here, complete enclosure is ophitic; record the observed boundaries and mineral identities when applying the distinction.

Field context Describe the observed section and distinguish host continuity from similar colour. A broken cutting may truncate a crystal boundary, and a two-dimensional view cannot establish every three-dimensional connection. This texture alone does not specify a cooling rate, magma source or permeability.

Worked example: crystal enclosure versus grain size

Also called: Subophitic

References & related terms

IODP Expedition 402 — Methods, igneous grain relationships Reference checked 2026-10-30

Additional interpretation reference

Related: Poikilitic texture · Ophitic texture · Plagioclase (Geology Dictionary) · Pyroxene · Porphyritic texture (Geology Dictionary)

View schematic: Crystal enclosure: poikilitic, ophitic and subophitic

Reservoir geology#

Assemblage biozone

A body of strata distinguished from neighbouring strata by a characteristic association of three or more fossil taxa. Recognition depends on the specified association, not necessarily on every member occurring in each sample.

Field context An individual member may range beyond the zone. Document the diagnostic association and reference section; do not redefine an assemblage biozone as the exact overlap of every member’s range.

Worked example: assemblage versus abundance evidence

Also called: Assemblage zone

References & related terms

International Commission on Stratigraphy — Biostratigraphic Units Reference checked 2026-10-31

Additional interpretation reference

Related: Biostratigraphy · Interval biozone · Concurrent-range zone · Abundance biozone

View schematic: Assemblage evidence versus abundance evidence

Reservoir geology#

Abundance biozone

A body of strata characterized by a notably higher abundance of a specified fossil taxon or group than in adjacent strata. Its boundaries follow marked changes in that abundance rather than the taxon’s complete range.

Field context State the counting basis and comparable sampling method. An abundance peak can reflect ecology or preservation and is not automatically synchronous between sections; a single rich sample does not establish a formally defined regional zone.

Worked example: assemblage versus abundance evidence

Also called: Abundance zone, Acme zone

References & related terms

International Commission on Stratigraphy — Biostratigraphic Units Reference checked 2026-10-31

Additional interpretation reference

Related: Biostratigraphy · Interval biozone · Concurrent-range zone · Assemblage biozone

View schematic: Assemblage evidence versus abundance evidence

Reservoir geology#

Lineage biozone

A body of strata containing fossils that represent a specified part of an evolutionary lineage. Its recognition requires supported evolutionary succession, not merely the appearance of different taxa in stratigraphic order; boundaries use the lowest occurrences of successive lineage elements.

Field context A lineage zone may cover only part of a taxon’s range. State the taxonomic and evolutionary evidence and the accepted occurrence criteria. A local lowest recorded occurrence is not automatically the evolutionary origin of the taxon; missing samples, reworking and drilling contamination must be assessed.

Worked example: lineage segment versus full taxon range

Also called: Lineage zone

References & related terms

International Commission on Stratigraphy — Biostratigraphic Units, lineage zones Reference checked 2026-10-31

Additional interpretation reference

Related: Interval biozone · Taxon-range zone · Biostratigraphy · Biohorizon

View schematic: A lineage segment is not necessarily a complete taxon range

Reservoir geology#

Barren interval

A stratigraphic interval lacking fossils. In biostratigraphy, barren intervals are not themselves fossil-defined units; they can lie between biozones or within one. A sample reported as barren records the outcome of an examination, not proof that every part of the interval is fossil-free.

Field context Record the fossil group sought, sample coverage and examination method. Distinguish no fossils recovered from no sample examined. Neither observation alone demonstrates a hiatus or supplies an age.

Worked example: zero recovery versus missing coverage

Also called: Fossil-barren interval

References & related terms

International Commission on Stratigraphy — Stratigraphic Guide, Chapter 7, barren intervals Reference checked 2026-10-31

Related: Biostratigraphy · Hiatus · Biohorizon

View schematic: Sampled zero is different from no sample

Geosteering & modelling#

Vertical exaggeration VE

The ratio of plotted vertical length per unit of real distance to plotted horizontal length per unit of real distance. Equal axis scales give VE = 1; VE greater than 1 stretches vertical relief and steepens the displayed slope without changing the geological geometry.

Field context Convert both axes to the same ground-distance units. For a straight section segment, tan(displayed angle) = VE × tan(actual section angle). Correct the plotted angle before interpreting dip; a section slope is true dip only when the section is aligned with the dip direction. Do not multiply the angle itself by VE.

Worked example: correcting a vertically exaggerated section

Also called: Vertical scale exaggeration

References & related terms

Saunders, Welch and MacKinnon — Physical Geography Laboratory Manual, Lab 15: vertical exaggeration Reference checked 2026-10-31

Related: Apparent dip · Formation dip

View schematic: Same section, two vertical scales

Wellsite geology & samples#

Compositional zoning

Variation in chemical composition between regions of a single crystal. In plagioclase, normal core-to-rim zoning trends toward lower anorthite component, while reverse zoning trends toward higher anorthite component. These describe compositional patterns, not unique temperature histories.

Field context Retain the traverse direction, analytical basis and spatial resolution. Core and rim measurements alone cannot reveal intervening oscillations. An optical band is an observation to investigate, not a chemical analysis or proof of a particular magma event.

Worked example: endpoints can hide crystal zoning

Also called: Crystal compositional zoning, Chemical zoning

References & related terms

Stephen A. Nelson, Tulane University — Tectosilicates Reference checked 2026-10-31

Additional interpretation reference

Related: Oscillatory zoning · Polysynthetic twinning · Mineral exsolution · Feldspar

View schematic: Plagioclase zoning: endpoints and internal variation

Wellsite geology & samples#

Oscillatory zoning

Repeated compositional increases and decreases across successive zones of a crystal. Oscillations can be superimposed on an overall core-to-rim trend, so a crystal may show both oscillatory and normal zoning. Distinguish chemical variation from the crystallographic orientation changes that define twinning.

Field context Retain the traverse direction, analytical basis and spatial resolution. Core and rim measurements alone cannot reveal intervening oscillations. An optical band is an observation to investigate, not a chemical analysis or proof of a particular magma event.

Worked example: endpoints can hide crystal zoning

Also called: Oscillatory crystal zoning

References & related terms

Smith and Lofgren (1983), Lithos — NASA technical record and abstract Reference checked 2026-10-31

Additional interpretation reference

Related: Compositional zoning · Polysynthetic twinning · Mineral exsolution · Feldspar

View schematic: Plagioclase zoning: endpoints and internal variation

Reservoir geology#

Bastite

A serpentine replacement aggregate that preserves features of an earlier pyroxene or amphibole grain, commonly an orthopyroxene. It is a textural name, not a separate mineral species.

Field context Document the evidence for the precursor separately from the minerals now present; inherited shape is not proof that pyroxene survives.

Worked identification: mesh cells are not original grains

Also called: Bastite texture

References & related terms

IODP Expedition 366 — Methods: serpentinite textures Reference checked 2026-10-31

Additional interpretation reference

Related: Pseudomorph · Mineral replacement · Pyroxene · Mesh texture

View schematic: Bastite and mesh: inherited texture clues

Reservoir geology#

Mesh texture

A netlike serpentinization texture with rims enclosing centres that may contain serpentine or residual olivine. Mesh-cell margins may follow fractures inside an original grain as well as its boundary.

Field context Do not count each mesh cell as one original olivine grain. Identify centre material rather than assuming that every centre is unaltered.

Worked identification: mesh cells are not original grains

Also called: Serpentine mesh texture

References & related terms

IODP Expedition 366 — Methods: serpentinite textures Reference checked 2026-10-31

Additional interpretation reference

Related: Pseudomorph · Mineral replacement · Olivine (Geology Dictionary) · Bastite

View schematic: Bastite and mesh: inherited texture clues

VISUAL REFERENCE

Oilfield schematics

Original conceptual illustrations. Select a term’s reference panel to find its related schematic.

An upright reference section has one fixed GSSP point. Two hypothetical numerical calibrations refer to that same point. A separate GSSA panel defines a boundary by an agreed numerical age.
Boundary definition and numerical calibration — Original GeoNavigate conceptual schematic, not to scale. The section and calibration values are invented; they do not depict a ratified locality or a measured result. Ma means millions of years before present. Open full-size · Concept references: stratigraphy.org · stratigraphy.org
Two upright beds: normal grading fines upward and inverse grading coarsens upward.
Normal and inverse sedimentary grading — Original GeoNavigate conceptual section: grain size decreases upward on the left and increases upward on the right. Stratigraphic top is known in this example. Not to scale; circles represent grains, not measured size distributions. Open full-size
Well geometry: along-hole and vertical depth. MD follows the borehole; TVD is measured vertically from the same datum. A simplified build and horizontal section show the difference.
Well geometry: along-hole and vertical depth — MD follows the borehole; TVD is measured vertically from the same datum. A simplified build and horizontal section show the difference. Conceptual; not to scale. Open full-size
The drilling-fluid circulation loop. Fluid travels down the drillstring, exits at the bit and carries cuttings up the annulus to surface solids-control equipment.
The drilling-fluid circulation loop — Fluid travels down the drillstring, exits at the bit and carries cuttings up the annulus to surface solids-control equipment. Conceptual; not to scale. Open full-size
A simplified cased-hole completion. Casing, cement, tubing, a packer and perforations have different functions. This conceptual arrangement does not represent every completion design.
A simplified cased-hole completion — Casing, cement, tubing, a packer and perforations have different functions. This conceptual arrangement does not represent every completion design. Conceptual; not to scale. Open full-size
SAGD: two wells, gravity drainage. Steam enters the upper well. Heated bitumen and condensed water drain toward the lower producer beneath the caprock.
SAGD: two wells, gravity drainage — Steam enters the upper well. Heated bitumen and condensed water drain toward the lower producer beneath the caprock. Conceptual; not to scale. Open full-size
CSS: one well, three operating phases. Steam injection, soaking and production occur sequentially through the same well. Actual cycles and well configurations vary.
CSS: one well, three operating phases — Steam injection, soaking and production occur sequentially through the same well. Actual cycles and well configurations vary. Conceptual; not to scale. Open full-size
Three-phase separation at surface. A conceptual vessel separates gas, oil and water into distinct outlet streams. Internal hardware and instrumentation are simplified.
Three-phase separation at surface — A conceptual vessel separates gas, oil and water into distinct outlet streams. Internal hardware and instrumentation are simplified. Conceptual; not to scale. Open full-size
Three approaches to artificial lift. Rod pumping, electric submersible pumping and gas lift use different mechanisms to help move well fluids to surface.
Three approaches to artificial lift — Rod pumping, electric submersible pumping and gas lift use different mechanisms to help move well fluids to surface. Conceptual; not to scale. Open full-size
Porosity and connected flow. Pores store fluids; connected pores and pore throats permit flow. Total porosity alone does not establish permeability. A separate proportional volume bar shows 75 cm³ solids and 25 cm³ pores in a hypothetical 100 cm³ sample.
Porosity and connected flow — Pores store fluids; connected pores and pore throats permit flow. Total porosity alone does not establish permeability. Conceptual; not to scale. Bottom bar: stipulated 100 cm³ bulk volume, 75% solids and 25% pores; this accounting bar does not show pore geometry. Concept reference: Groundwater Project, Basic Hydrogeology §3.2. Open full-size
Bedding dip and thickness. True stratigraphic thickness is measured normal to bedding. Vertical thickness differs in dipping strata. The illustrated relationship assumes parallel planar beds.
Bedding dip and thickness — True stratigraphic thickness is measured normal to bedding. Vertical thickness differs in dipping strata. The illustrated relationship assumes parallel planar beds. Conceptual; not to scale. The separate numerical example uses 30° dip; it does not specify the sketch angle. See the linked thickness worked example and University of Alberta primary-structures reference. Open full-size
Bent-motor drilling: slide and rotate. With a conventional bent motor, sliding holds a toolface orientation while the motor turns the bit. Surface rotation sweeps the bend around the hole. Rotary-steerable systems operate differently.
Bent-motor drilling: slide and rotate — With a conventional bent motor, sliding holds a toolface orientation while the motor turns the bit. Surface rotation sweeps the bend around the hole. Rotary-steerable systems operate differently. Conceptual; not to scale. Open full-size
Well-control equipment identification. A conceptual annular and ram preventer stack, accumulator and choke/kill connections. Equipment identification only; configurations and capabilities vary.
Well-control equipment identification — A conceptual annular and ram preventer stack, accumulator and choke/kill connections. Equipment identification only; configurations and capabilities vary. Conceptual; not to scale. Open full-size
Incident, reflected and transmitted P-wave paths at an interface, with normal-incidence reflection coefficient equation. A separate lower example gives two density–velocity pairs with equal impedance and zero ideal normal-incidence reflection.
Acoustic impedance and seismic reflection — At normal incidence, the signed P-wave amplitude reflection coefficient depends on the acoustic impedances across a boundary. Paths are offset for clarity. Original conceptual illustration; not to scale. Lower numerical example is a separate equal-impedance case; it does not use the reflected arrow in the upper conceptual diagram. Open full-size · Concept references: glossary.slb.com · glossary.slb.com
A plan-view fracture with proppant grains and arrows showing reservoir fluid moving toward a well.
A propped fracture connects rock to the well — Fluid enters a conductive fracture from reservoir rock and moves along it toward the well. Proppant helps retain a flow path. Plan view; aperture exaggerated; actual fracture geometry varies. Original conceptual illustration. Open full-size · Concept references: glossary.slb.com · www.slb.com
Qualitative oil and water relative-permeability curves against increasing water saturation, with oil reaching zero at residual oil saturation.
Two fluids share the same pore network — Illustrative oil–water relative-permeability curves show how the ability of each phase to flow changes with water saturation. Shape and endpoints depend on rock, fluids and displacement history; no measured values are implied. Open full-size · Concept references: glossary.slb.com · glossary.slb.com
Wellstream enters a separator and branches to gas dehydration, oil treatment and water treatment before further handling.
From wellstream to separate process streams — A three-phase separator splits bulk gas, oil and water. Gas dehydration removes water vapor; oil and water may need further treatment. Selected process relationships only, not a facility design or operating procedure. Open full-size · Concept references: glossary.slb.com · glossary.slb.com · glossary.slb.com
Looking downhole at a circular cross section, gravity toolface is zero at high side, 90 degrees right, 180 degrees low side and 270 degrees left.
Gravity toolface: looking downhole — Clockwise angles around the borehole axis: high side 0°, right 90°, low side 180°, left 270°. Magnetic toolface uses a different reference. High side is poorly defined near vertical. Conceptual; not an operating instruction. Open full-size · Concept references: glossary.slb.com
Three arrows from a common origin indicate true north, grid north and magnetic north; captions distinguish declination and convergence.
True, grid and magnetic north — Three distinct reference directions at one location. Declination relates true and magnetic north; convergence relates true and grid north. Arrow positions are illustrative, not local survey values. Open full-size · Concept references: www.usgs.gov
Survey stations constrain endpoint directions; a smooth path and a more variable path illustrate unresolved between-station curvature.
A survey is sampled; the path is reconstructed — Measured directions constrain the well at survey stations. A smooth reconstruction can miss smaller bends between stations. The curves are conceptual and do not represent a calculated or surveyed well. Open full-size · Concept references: www.iscwsa.net
Two piezometers show head falling from 102 metres to 100 metres over 100 metres; flow points toward lower head. For the same flux, flow porosities of 0.10 and 0.25 give 100-day and 250-day bulk travel estimates over 100 metres.
Groundwater head loss and Darcy flux — Original GeoNavigate schematic. Horizontal saturated, homogeneous, isotropic aquifer segment; equal-density water and steady one-dimensional flow. Heads share one datum. Conceptual, not to scale. Sensitivity labels hold K and gradient fixed while varying effective flow porosity; times are bulk advection estimates, not first arrival. Open full-size · Concept references: books.gw-project.org · fc79.gw-project.org
North–south strike, eastward dip and a northeast section heading; two profiles compare 30 degree true dip with 16.1 degree apparent dip. A separate lower plan plots east and north slope components 0.3 and 0.4, whose resultant magnitude is 0.5.
Strike, dip direction and apparent dip — Original GeoNavigate conceptual schematic. Plan arrows show headings, not distances. Profile geometry uses equal horizontal and vertical scales: a 30° plane drops 57.7 m over 100 m east, but only 28.9 m over 100 m toward 030°. No measured well data. Lower panel: separate hypothetical gradient-vector construction with equal component scales; arrows encode slopes, not map distances. Open full-size · Concept references: pressbooks.openeducationalberta.ca · www.cambridge.org
A phi scale with halving diameters, two contrasting size spreads, and angular equant versus rounded elongated grain outlines. An added example compares eight small spheres and one sphere of double diameter: equal total mass despite unequal counts. A lower comparison gives 0.25 mm from mean phi versus 0.3125 mm from arithmetic mean diameter, with proportional bars.
Grain size, sorting and grain shape — Original GeoNavigate conceptual illustration, not to scale. Equal spacing on the phi axis represents a factor of two in diameter. Shape silhouettes illustrate distinctions, not quantitative sphericity measurements. The added hypothetical sphere example assumes equal density: doubling diameter multiplies volume and mass by eight; counts and mass percentages differ. Lower bars compare two equally weighted observations; bar lengths scale with the stated mean diameters. Open full-size · Concept references: publications.iodp.org · www.open.edu · www.nhm.uio.no
Parallel horizontal traces count as one cleavage direction; perpendicular horizontal and vertical traces count as two; curved fracture surfaces do not define cleavage.
Cleavage directions versus fracture — Original GeoNavigate conceptual sections, not to scale. Two-dimensional traces illustrate orientation families, not crystal habit or a measured specimen. Open full-size · Concept references: www2.tulane.edu · learningzone.web.ox.ac.uk
Three conceptual stages: initial burial in an older bed, erosion and transport, then incorporation of an older fossil into younger sediment.
Fossil reworking: two burial histories — Original GeoNavigate conceptual sequence, not to scale. Left to right is event order, not distance. The fossil predates its second host bed; its age alone does not date that bed. No measured ages or private samples are shown. Open full-size · Concept references: www.nps.gov · pubs.usgs.gov
Two horizontal layers with impedances 6 and 9 million kilograms per square metre per second; downward incident and upward reflected paths give a positive pressure reflection coefficient of 0.20. A lower panel distinguishes transmitted pressure ratio 1.20 from energy fractions 4 percent reflected and 96 percent transmitted.
Normal-incidence reflection at an impedance contrast — Original GeoNavigate conceptual cross-section, not to scale. Invented homogeneous layers; ray paths separated for readability. Pressure-amplitude convention R = (Z2 − Z1)/(Z2 + Z1); no measured seismic trace is shown. The lower energy bar is proportional: 4% reflected plus 96% transmitted; pressure amplitudes are not energy fractions. Open full-size · Concept references: www.eoas.ubc.ca · www.eoas.ubc.ca · staff.washington.edu
Equal-length bars show parent fractions 100, 50, 25 and 12.5 percent at zero through three half-lives, with complementary radiogenic daughter fractions. A second comparison holds parent at 125 ratio units while radiogenic daughter decreases from 875 to 437.5. A separate proportional bar shows 75% parent and 25% daughter at 0.415 half-lives. A lower scaled axis compares ages 29.260, 30.000 and 30.704 million years from daughter/parent ratios 6.6, 7.0 and 7.4.
Radioactive decay in a closed teaching system — Original GeoNavigate conceptual schematic. Bar fractions are quantitative; no spatial or geological time scale is implied. Invented single-step decay system, zero initial daughter and no isotope exchange. Lower panel: invented daughter loss immediately before measurement, with parent unchanged; absolute bar lengths share one ratio-unit scale. Bottom bar: original fractional-half-life calculation, with the same 560-pixel full-inventory scale. The lower panel maps stipulated ratio bounds through a nonlinear age equation with an exact illustrative half-life; it does not depict statistical confidence limits. Open full-size · Concept references: pubs.usgs.gov · opentextbc.ca · www.homepages.ucl.ac.uk · www.homepages.ucl.ac.uk
Two equal total-stress bars show pore pressure falling from 120 to 80 kilopascals and effective stress rising from 80 to 120 kilopascals. A separate section shows a water table falling from the surface to 5 m depth above a fixed observation point at 10 m.
Effective stress during pore-pressure decline — Original GeoNavigate conceptual schematic. Invented saturated-soil example with constant total vertical stress, compression positive and Terzaghi coefficient one. Bar lengths show stress, not layer thickness; not a geological section. Lower panel: separate idealized hydrostatic states; drained upper sediment has lower bulk unit weight. Depth increases downward; geometry is conceptual and not to scale. Open full-size · Concept references: environment.uwe.ac.uk · books.gw-project.org · books.gw-project.org
Ideal tube comparison: radius ten micrometres gives six kilopascals; radius two micrometres gives thirty kilopascals at identical tension and wetting. A separate input check shows that diameter ten micrometres means radius five micrometres and twelve kilopascals.
Pore-throat radius and capillary entry — Original GeoNavigate ideal cylindrical-throat comparison, not to spatial scale. Invented values, water-side contact angle zero, interfacial tension 0.030 N/m. No measured core or seal capacity is implied. The lower input check uses diameter, not the radius of Case A. Open full-size · Concept references: mooseframework.inl.gov · openpnm.org
Two piezometer levels above the aquifer roof show a two metre head decline while the aquifer remains saturated. A separate two-zone example releases 1 and 3 cubic metres from equal areas with different head declines.
Confined aquifer: head decline and stored water — Original conceptual section, not to scale. Invented uniform head change; the water levels are piezometric levels, not a falling water table inside the confined aquifer. Small elastic deformation is omitted from geometry. Lower panel: independent two-zone calculation; rectangles represent equal plan areas, not aquifer cross-section geometry. Open full-size · Concept references: books.gw-project.org · books.gw-project.org
Identical conceptual saturated pore networks with twice the viscosity in fluid B give half the conductivity and specific discharge at fixed density and gradient. A lower panel shows equivalent calculations using dynamic and kinematic viscosity.
Same pore network, different hydraulic conductivity — Original GeoNavigate conceptual schematic, not to spatial scale. Hypothetical single-phase Darcy-flow calculation; bar lengths represent the calculated 2:1 conductivity ratio, not measured reservoir results. Lower panel converts dynamic viscosity to kinematic viscosity for fluid A; both equation forms give the same conductivity. Open full-size · Concept references: books.gw-project.org · www.grc.nasa.gov
Flat overlapping clasts dip toward upstream on the left while flow points right; a hypothetical westward clast dip gives eastward inferred flow.
Clast imbrication and inferred flow — Original GeoNavigate conceptual vertical section, not to scale. Horizontal bedding and an upstream-dipping fabric are assumed. The 270°/090° example is invented, not a measured dataset or a figure from the cited paper. Open full-size · Concept references: onlinelibrary.wiley.com · www.usgs.gov · circstat.github.io
Two proportional volume bars for a hypothetical one cubic metre sample. Initially 0.70 cubic metres of solids and 0.30 of water; after drainage, 0.70 solids, 0.12 retained water and 0.18 air. Collected water is 0.18 cubic metres. Lower panel compares cumulative drainage of 0.10 m³ at 1 hour and 0.18 m³ at 24 hours, with 0.20 and 0.12 m³ water remaining.
Gravity drainage: account for all the water — Original conceptual volume accounting, not a geological cross-section or measured result. Bar widths represent volume fractions, not pore geometry. Fixed bulk volume; initially all pores water-filled, no isolated pores, evaporation or solid deformation. Drainage endpoint must be specified. Lower panel is a separate invented finite-duration comparison; no equilibrium endpoint or time interpolation is implied. Open full-size · Concept references: water.usgs.gov · www.usgs.gov · books.gw-project.org
A conceptual vertical profile places saturated capillary-fringe water above the zero-gauge-pressure water table. At equilibrium, a point 0.50 metres above has pressure head minus 0.50 metres; a point 1.00 metre below has pressure head plus 1.00 metre.
Capillary fringe: saturation is not pressure — Original GeoNavigate conceptual section, not to spatial scale. Hypothetical hydrostatic water column, constant density and atmospheric air pressure. Water table is the zero gauge-pressure surface; the capillary-fringe top is a separate, material-dependent boundary. No field measurements or reproduced artwork. Open full-size · Concept references: courses.ems.psu.edu · books.gw-project.org
Two parallel five-level hierarchies pair eonothem with eon, erathem with era, system with period, series with epoch, and stage with age, from broader to finer principal rank; subsidiary ranks are omitted.
Chronostratigraphic rocks and geochronologic time — Original GeoNavigate hierarchy schematic. Box widths indicate principal rank order only, not duration or rock thickness; conceptual and not to scale. Open full-size · Concept references: stratigraphy.org · stratigraphy.org
Time-position diagram with younger ages upward. A rock boundary rises from 100 Ma in the west to 98 Ma in the east, crossing the horizontal 99 Ma time surface. The vertical axis is time, not depth.
A rock boundary can cross time surfaces — Original GeoNavigate conceptual illustration, not to scale. Ages and locations are invented, not measured. Ma means millions of years before present; horizontal lines represent equal age, not horizontal beds. Open full-size · Concept references: stratigraphy.org · stratigraphy.org
Conceptual rock column with upper and lower significant unconformities enclosing a candidate synthem of three beds; a short internal pause is marked separately. Younger strata are upward.
Synthem boundaries and an internal depositional pause — Original GeoNavigate conceptual column, not to scale. It illustrates the boundary test for a candidate synthem; bed thicknesses and break durations are unspecified, and no measured or formally named unit is shown. Open full-size · Concept references: stratigraphy.org
A conceptual downward-closing angular fold has a west limb dipping 30 degrees east and an east limb dipping 50 degrees west. Their interlimb angle is 100 degrees. Bed ages are unspecified. Lower comparison: a 45-degree-to-strike vertical section shows apparent limb dips 22.2 and 40.1 degrees, giving a 117.7-degree section angle.
Fold profile: shape, limb angle and bed age — Original GeoNavigate teaching schematic. Angles are drawn to the stated values; no spatial scale, thickness or measured data is implied. Shape establishes a synform; relative bed ages are separate evidence. Lower panel is an oblique vertical section, not the fold profile; calculated angles use equal horizontal and vertical scales. Open full-size · Concept references: opentextbc.ca · pressbooks.openeducationalberta.ca · pressbooks.openeducationalberta.ca
Two horizontal three-bed stacks: upright beds young upward from 120 to 100 Ma; overturned beds young downward from 120 to 100 Ma. Arrows distinguish present vertical from stratigraphic younging.
Present vertical and stratigraphic younging — Original GeoNavigate conceptual schematic, not to scale. Invented depositional ages illustrate independently established order; they are not measurements. The panels are end-member orientations, not a reconstruction of a specific fold. Open full-size · Concept references: pressbooks.openeducationalberta.ca · opentextbc.ca
Three conceptual panels compare an intersection lineation formed by bedding and cleavage, a crenulation lineation defined by small-fold hinges, and a stretching lineation defined by elongated objects. An invented trend and plunge example keeps the three observations separate before interpretation.
Lineation mechanisms and interpretation checks — Original GeoNavigate conceptual schematic, not to scale. The example orientations are invented teaching values, not measured attitudes. Similar trends do not prove a common origin, and a stretching lineation is not automatically a movement direction. Open full-size · Concept references: pressbooks.openeducationalberta.ca · www.diogenes.uni-potsdam.de
Plan view shows a northeast trend of 030 degrees clockwise from north; a vertical section along that trend shows a 20 degree downward plunge and a 3.64 metre drop over 10 metres horizontally.
Trend and plunge: two views of one line — Original GeoNavigate teaching diagram. Invented 030°/20° orientation; conceptual, not a measured section or spatial scale. Arrowheads identify the downward end, not movement sense. Open full-size · Concept references: gq.mines.gouv.qc.ca
Conceptual cross-section shows a narrow fault core between fractured damage zones and less-deformed wall rock. A separate fault-surface view shows parallel slickenlines with two opposed arrows to indicate that lineation alone gives direction but not slip sense.
Fault-zone architecture and slip-direction evidence — Original GeoNavigate conceptual schematic, not to scale. Widths, fracture density and symmetry are illustrative. Blue arrows show possible along-zone flow; the dashed cross-fault arrow is a caution, not a measured permeability result. Slickenlines indicate a line of movement, not displacement magnitude or sense by themselves. Open full-size · Concept references: pressbooks.openeducationalberta.ca · webapps.bgs.ac.uk · webapps.bgs.ac.uk
Plan view of two joint sets, beside parallel fracture walls with a normal width b and a longer oblique measurement L.
Joint sets and normal aperture — Original GeoNavigate conceptual schematic, not to spatial scale. The invented aperture example uses parallel walls: b = L cos theta, where theta is measured from the wall normal. Joint traces do not establish flow connectivity or age. Open full-size · Concept references: pressbooks.openeducationalberta.ca · opentextbc.ca
Three conceptual sections show an open fracture, mineral fill occupying that space, and a later opening within the fill. Blue marks void and ochre marks solid mineral.
Opening, mineral filling and reopening — Original GeoNavigate conceptual sequence, not to scale. Panels illustrate a possible history, not measured stages or diagnostic proof of crack-seal growth. Mineral fill is solid; its thickness is not present-day open aperture. Open full-size · Concept references: pressbooks.openeducationalberta.ca
Conceptual section shows a narrow ductile shear zone containing an S foliation, C surfaces, a later C-prime shear band, stretched clasts and a grain-size gradient. A comparison panel separates dynamically recrystallized mylonite from fragmental cataclasite.
Ductile shear-zone fabric and brittle–ductile distinction — Original GeoNavigate conceptual schematic, not to scale. Fabric angles, clast shapes, grain sizes and zone width are illustrative; arrows show a possible dextral interpretation only for this drawing. The figure contains no measured section, core or thin-section data. Open full-size · Concept references: pressbooks.openeducationalberta.ca · opentextbc.ca · earthwise.bgs.ac.uk
Three conceptual thin-section panels compare a grown porphyroblast, a relict porphyroclast in a finer deformed matrix, and a core-and-mantle structure with fine recrystallized grains surrounding a strained core.
Porphyroblast, porphyroclast and recrystallized mantle — Original GeoNavigate conceptual thin-section schematic, not to scale. Grain shapes, sizes, foliation and the invented 1.20 mm to 0.08 mm size comparison are illustrative, not measured material or a temperature, stress or strain calibration. Open full-size · Concept references: pressbooks.openeducationalberta.ca · webapps.bgs.ac.uk · www.iodp.tamu.edu
Two equal-length percentage bars show an invented protomylonite with 65 percent porphyroclasts and an ultramylonite with 5 percent porphyroclasts. Thresholds are greater than 50 percent and less than 10 percent respectively.
Porphyroclast-volume classification: two end members — Original GeoNavigate classification schematic. Bar lengths are proportional to invented volume percentages; this is not a geological section or a grain-size drawing. No measured sample, deformation trajectory or strain calibration is represented. Open full-size · Concept references: webapps.bgs.ac.uk · webapps.bgs.ac.uk
Two separate experiments through the same two horizontal layers: parallel flow gives K of 8.2 metres per day; perpendicular flow gives about 3.571 metres per day. The thinner low-conductivity layer produces most of the perpendicular head loss.
Layer-parallel and layer-normal groundwater flow — Original GeoNavigate conceptual cross-sections, not to spatial scale. Invented inputs, steady saturated flow and continuous homogeneous isotropic layers. Arrows indicate separate imposed flow directions, not relative discharge magnitudes. No measured well or publication figure is shown. Open full-size · Concept references: books.gw-project.org · books.gw-project.org · ngwa.onlinelibrary.wiley.com
Separate conceptual underside views show a flute with a bulbous upstream end and fading downstream tail, and straight groove ridges with a two-way alignment. A section shows sand filling a scour in mud.
Flute casts and groove casts: direction versus axis — Original GeoNavigate conceptual illustration, not to scale. Separate examples, not a single measured bed or a reproduced publication figure. The two-headed groove arrow denotes unresolved flow sense, not reversing flow. The section uses depositional up; underside views have no compass orientation. Open full-size · Concept references: sites.ualberta.ca · onlinelibrary.wiley.com
Upright conceptual cross-section: two sand lobes project down into mud, with a narrow mud tongue extending upward between them. A dashed reference contact separates positive-up and negative-down offsets.
Load casts and flame structures at a sand–mud contact — Original GeoNavigate conceptual illustration, not to scale; not a publication figure or measured result. Arrows identify sediment geometry, not flow direction. The reference contact is assumed for this teaching example, not reconstructed from an actual bed. Open full-size · Concept references: pressbooks.openeducationalberta.ca · onlinelibrary.wiley.com
Two conceptual upright sections compare laminae folded within a bounded bed with folded beds in a candidate slump interval. Undisturbed layers bracket each example; no movement direction is inferred.
Convolute lamination and a candidate slump fold — Original GeoNavigate schematic, conceptual and not to scale. Shapes are explanatory, not measured core or a publication figure. The right panel requires independent evidence of soft-sediment downslope movement before classification as a slump fold. Open full-size · Concept references: publications.iodp.org · sites.ualberta.ca
An upright conceptual sediment section shows concave-up dish laminae interrupted by a steep pale pillar. A separate upward arrow indicates interpreted water escape, not measured velocity.
Dish laminae and a pillar — Original GeoNavigate conceptual schematic, not to scale. Geometry illustrates terminology, not a measured core or a reproduced publication figure. Arrows show an interpretation; they do not identify the trigger or depositional environment. Open full-size · Concept references: archives.datapages.com · sites.ualberta.ca
Conceptual plane-polarized colour comparison and crossed-polar views at zero, forty-five and ninety degrees. A separate invented stage-reading calculation gives fifteen degrees.
Absorption colour and crossed-polar extinction — Original GeoNavigate conceptual schematic, not to scale. Colours and brightness are illustrative, not measured mineral responses or a publication figure. Stage readings are invented teaching values. Open full-size · Concept references: www2.tulane.edu · www2.tulane.edu
An illustrative temperature versus age plot runs toward the present to the right. A prescribed straight segment joins 180 degrees Celsius at 20 million years ago to 80 degrees Celsius at 10 million years ago, giving an average cooling magnitude of 10 degrees Celsius per million years.
An invented cooling interval — Original GeoNavigate conceptual teaching plot, with labelled numerical axes and invented values; not a spatial section or measured result. The straight segment is prescribed for arithmetic, not inferred from two dates. No mineral-specific closure temperatures are assigned. Open full-size · Concept references: pieter-vermeesch.es.ucl.ac.uk · esurf.copernicus.org · cutrail.org
A hypothetical upright core has normal, reversed and normal polarity downwards. Two invented age windows share this pattern. An independent age bracket at the middle level accepts candidate A and rejects candidate B.
A polarity pattern needs an age anchor — Original GeoNavigate conceptual schematic; not to scale. N and R are interpreted polarity labels, not measured vectors. Depth increases downward; both candidate age axes increase downward. All ages are invented; no real chron is assigned. Open full-size · Concept references: stratigraphy.org · nacsn.americangeosciences.org · publications.iodp.org
An invented one-litre sample contains 600 cubic centimetres of solids, 250 of water and 150 of air. A volume bar and four formulas compare porosity 0.40, void ratio 0.667, water content 0.25 and saturation 0.625.
One sample, four different volume ratios — Original GeoNavigate conceptual volume-accounting schematic. Bar widths are proportional to the invented volumes; this is not a geological section or measured sample. Spatial geometry is not to scale. No publication artwork reproduced. Open full-size · Concept references: books.gw-project.org · books.gw-project.org
Conceptual reversible exchange between dissolved and sorbed solute, with an invented transport calculation: water speed 0.40 metres per day, retardation factor 4 and solute speed 0.10 metres per day. A proportional distance axis shows 100 and 25 metres after 250 days.
Water movement and reversible sorption — Original GeoNavigate conceptual schematic and hypothetical calculation, not measured results or a publication figure. Pore geometry is not to scale; the labelled distance axis is quantitative. No degradation or dispersion is modelled. Open full-size · Concept references: books.gw-project.org · nepis.epa.gov · books.gw-project.org
Three conceptual pattern maps compare parallel twin bands, crossing twin bands and a grain with no resolved internal pattern. The last observation remains unresolved rather than being assigned to quartz.
Feldspar twin patterns and an unresolved grain — Original GeoNavigate conceptual pattern maps, not to scale and not microscope images. Shades distinguish domains; they do not simulate interference colours or a measured stage orientation. No publication figure reproduced. Open full-size · Concept references: www2.tulane.edu · tmi.laccore.umn.edu · www.nmnhs.com · www2.tulane.edu
At a fixed invented velocity of 3000 metres per second, 30 and 60 hertz give wavelengths of 100 and 50 metres. Quarter-wavelength reference lengths are 25 and 12.5 metres, shown on a shared quantitative length axis. Two original calculated traces below compare 4 and 16 millisecond reflection separations at the same frequency and amplitude scale.
Wavelength and a quarter-wavelength separability estimate — Original GeoNavigate teaching calculation. Bars are quantitative lengths, not a geological cross-section or simulated seismic trace. Values are hypothetical; quarter-wavelength estimates do not guarantee field resolution. No measured data or publication artwork. Added synthetic panels use a 30 Hz Ricker wavelet and coefficients +0.2 and −0.2 at separations of 4 and 16 ms. Shared amplitude scale; dashed lines mark interface times, not picked extrema. Open full-size · Concept references: www.eoas.ubc.ca · www.jstage.jst.go.jp · www.epa.gov
Two conceptual sections compare a sharp-walled burrow in firm unlithified sediment with a boring that cuts an already cemented surface. Both are capped by later sediment; time of cementation is the key distinction.
Firm and lithified substrates at colonization — Original GeoNavigate conceptual sections, not to scale. Substrate state refers to colonization time, not present hardness. Generic trace shapes are not taxonomic identifications; no measured data or publication artwork. Open full-size · Concept references: ichnology.ku.edu · www.sepmstrata.org · geojournals.pgi.gov.pl
A section normal to idealized fold hinges shows folded earlier foliation in cyan, later axial-surface traces in orange, and hinge lines as dots pointing out of the section.
Earlier foliation, later cleavage and hinge lineation — Original GeoNavigate conceptual geometry, not to scale. S1 and S2 are local fabric-order labels; dots show lines normal to this section. No compass, depth or measured strain is implied. Not a reproduced publication figure. Open full-size · Concept references: blogs.egu.eu · blogs.egu.eu · pressbooks.openeducationalberta.ca
Two idealized vertical profiles normal to ripple crests. An asymmetric current ripple has a gentle stoss slope and steep lee slope to the right. A symmetric wave-ripple example has arrows in both directions. Shapes are end members, not diagnostic templates.
Ripple profiles: current direction and oscillation axis — Original GeoNavigate conceptual schematic, not to scale. Arrows show idealized near-bed flow, not wave propagation or measured transport. No compass orientation or depth is implied. Internal laminae are omitted. Wave ripples need not be symmetric; combined flow and bed slope complicate interpretation. Open full-size · Concept references: blogs.egu.eu · www.nps.gov · repository.tudelft.nl
Two conceptual sections: coarse fragments touch in a framework on the left; isolated fragments lie in finer material on the right. Leader lines identify a clast contact and surrounding finer material.
Clast support versus matrix support — Original GeoNavigate conceptual schematic, not to scale. Tan background represents finer sediment, not measured porosity. No flow direction, depth or gravitational loading is implied. Ideal circular fragments simplify a three-dimensional fabric; a real section may miss out-of-plane contacts. Open full-size · Concept references: publications.iodp.org · rocksminerals.flexiblelearning.auckland.ac.nz
Three ideal sections show parent mineral A, a remnant A core surrounded by product B, and B occupying the same outer outline. Arrows indicate a possible sequence, not fluid flow.
Replacement with an inherited outline — Original GeoNavigate conceptual schematic, not to scale. A and B are generic mineral identities, not chemical formulas or measured phases. The same outline illustrates one possible shape-preserving replacement; it does not imply constant mass, reaction rate or porosity. No crystallographic orientation or depth is assigned. Open full-size · Concept references: website.whoi.edu · qrius.si.edu · digital.library.adelaide.edu.au
Plan-view direction sketch: the negative head gradient points 45 degrees from positive x, while Darcy flux points 5.71 degrees from positive x for conductivity components 10 and 1 metres per day.
Head-drop direction and Darcy flux — Original conceptual plan-view direction schematic with hypothetical inputs. Not to spatial scale; angles are drawn geometrically. Arrows show directions only and use independent lengths because gradient and flux have different units. Local principal axes x and y are not compass bearings; no depth or measured field result is represented. Open full-size · Concept references: books.gw-project.org · fc79.gw-project.org · books.gw-project.org
An upright conceptual section shows sandstone containing a defensible 105 Ma detrital population below primary ash dated 100 Ma. A numerical-age axis decreases rightward from 110 to 95 Ma; the permissible depositional-age bracket lies between 105 and 100 Ma.
A maximum depositional age is a bound — Original GeoNavigate teaching schematic with invented exact ages. Section and grain symbol are not to scale; the age axis is linear. No depth, measured sample or published-author figure is represented. The 100–105 Ma bracket assumes intact superposition, a valid pre-depositional grain age and an eruption-age primary ash. Analytical uncertainty is omitted only for this exercise. Open full-size · Concept references: www.saskoer.ca · www.usgs.gov · experts.arizona.edu
Two conceptual upright sections: sand with short mud streaks in ripple troughs on the left, and separated sand lenses in continuous mud on the right. Colours and labels identify sand and mud; no current direction is assigned.
Flaser and lenticular bedding: trace the contrasting material — Original GeoNavigate conceptual schematic, not to scale. Idealized two-dimensional sections illustrate bedding geometry; they are not measured core or reproduced publication figures. Internal ripple laminae are omitted. No flow direction, time interval, sand percentage or three-dimensional connectivity is implied. Open full-size · Concept references: www.kgs.ku.edu · www.kgs.ku.edu · onlinelibrary.wiley.com
Equal-scale coordinates within a fault plane show cutoff A at y equals x and cutoff B at y equals x plus four metres. Two arrows from P, zero comma four and three comma seven metres, both reach B. A separately matched point Q selects the latter vector.
One marker offset, multiple possible slip vectors — Original GeoNavigate conceptual illustration with invented coordinates, not measured data or a publication figure. The fault-plane plot uses equal metre scales; its geographic setting is not to scale and no compass bearing or vertical depth is assigned. Arrows are alternative relative translations, not successive movements. P and Q are only a matched pair when independent marker evidence establishes the correspondence. Added projection labels assume a 30° fault dip; down-dip distance and vertical displacement remain distinct. Open full-size · Concept references: pressbooks.openeducationalberta.ca · psgt.earth.lsa.umich.edu
Two invented equilibrium cases have melt concentration ten milligrams per kilogram. Mineral A has two and coefficient 0.2; mineral B has forty and coefficient four. A one-kilogram B crystal fraction holds forty milligrams, while nine kilograms of melt hold ninety milligrams. A lower panel converts 75:25 volume proportions to 69.23:30.77 mass percentages using different densities.
Partition coefficient compares concentrations, not inventories — Original GeoNavigate conceptual schematic with invented concentrations and phase masses, not measured data or a reproduced publication figure. Phase boxes are not to scale; their areas do not represent mass or volume. A and B are separate hypothetical cases. No transport arrows, depth, time sequence or named-element coefficient is implied. Lower panel is a separate hypothetical solid assemblage; bar lengths encode volume and mass percentages respectively, not spatial geometry. Open full-size · Concept references: primer-computational-mathematics.github.io · agupubs.onlinelibrary.wiley.com
Six invented shells died 1000, 800, 600, 400, 200 and zero years before sampling. All enter one sample containing two hypothetical taxa. The numerical time axis is linear; positions in the sample box are arbitrary.
One sample can contain several death times — Original GeoNavigate conceptual example, not measured ages or a reproduced publication figure. Time axis is linear; shell sizes and sample geometry are not to scale. Labels A and B are hypothetical taxa. The connecting arrow means collection into one sample, not a sediment-transport direction or burial history. Open full-size · Concept references: www.kgs.ku.edu · www.digitalatlasofancientlife.org · onlinelibrary.wiley.com
Conceptual plan view of a tracer patch spreading along and across rightward mean flow. Separate calculation panels show a 40 m average advective displacement in 100 days and mechanical coefficients of 0.8 and 0.08 square metres per day. A lower panel shows concentration decreasing from 2.0 to 0.5 mol per cubic metre over 0.10 m and positive diffusive flux without mean water flow.
Solute movement and spreading are different quantities — Original GeoNavigate conceptual illustration with invented inputs. Plan view, no depth axis; geometry and arrow lengths are not to scale. Outlines are illustrative patches, not concentration contours or calculated plume boundaries. No measured result or reproduced source figure. The lower panel uses a stated free-water coefficient; the concentration graph has labelled axes and is not a geological cross-section. Open full-size · Concept references: books.gw-project.org · courses.ems.psu.edu · water.usgs.gov · fc79.gw-project.org · courses.ems.psu.edu
Conceptual sections show a homogeneous alkali feldspar becoming a potassium-rich host containing three sodium-rich lamellae. Separate labels explain that the arrow indicates a possible cooling sequence, while colours indicate composition rather than microscope interference colours.
Solid-state unmixing in alkali feldspar — Original GeoNavigate conceptual explanation, not a publication figure or measured specimen. Sections, lamellar widths and spacing are not to scale; no crystallographic orientation, temperature or cooling duration is assigned. Composition colours are symbolic, not optical colours. Open full-size · Concept references: serc.carleton.edu · link.springer.com · doi.org
Two invented vertical sediment sections contrast surviving horizontal lamination cut by two burrows with overlapping burrows and patchy surviving lamination. A separate panel lists observations needed before an ichnofacies interpretation. No numerical intensity class is assigned to either sketch. A lower numerical panel shows an invented 28–34 percent estimate crossing the 30 percent threshold between Expedition 403 codes 1 and 2.
From core fabric to environmental interpretation — Original GeoNavigate conceptual sections, not measured cores or reproduced publication figures. Geometry, burrow dimensions and spacing are not to scale. Up indicates section top only; no geographic orientation, depth, age or water-depth scale is supplied. Panels are independent examples, not a time sequence or index calibration. Lower panel: original numerical uncertainty example, not a core image or full index chart; percentage-axis positions are proportional. Open full-size · Concept references: publications.iodp.org · www.uky.edu · publications.iodp.org
An initial circle of radius 60 drawing units is compared with ellipse A of semiaxes 90 and 40 and ellipse B of semiaxes 135 and 60. Both ellipses have a major-to-minor ratio of 2.25, but their areas relative to the circle are 1 and 2.25.
Equal shape ratio does not mean equal area change — Original GeoNavigate mathematical teaching diagram with invented stretches. Circle and ellipse dimensions share the same drawing scale; panel spacing and geological setting are not to scale. A and B are alternative final states, not successive steps. No measured rock, geographic orientation, depth, stress or elapsed time is represented. Sources explain the concepts; this is not a reproduced author figure. Open full-size · Concept references: pressbooks.openeducationalberta.ca · psgt.earth.lsa.umich.edu
Two cosine curves, 180 hertz and 70 hertz, pass through the same eleven sample points at 4 millisecond intervals from 0 to 40 milliseconds. The sample frequency is 250 hertz and the Nyquist frequency is 125 hertz.
Different signals can have identical samples — Original GeoNavigate mathematical teaching diagram, not measured seismic data or a reproduced publication figure. Time and dimensionless amplitude use the labelled linear axes. The geological setting and layout are conceptual, not to scale; no depth, velocity or compass orientation is represented. Curves are alternative continuous signals, not successive processing steps. Open full-size · Concept references: www.eoas.ubc.ca · wiki.seg.org · sep.stanford.edu
Left: four unchanged round grains pack closer together. Right: two grains meet at a flattened dissolution contact under opposed loading arrows; a dashed arrow indicates possible solute transport away from that contact.
Mechanical packing and pressure solution — Original GeoNavigate conceptual grain-scale schematic, not to scale and not a measured sample or reproduced publication figure. Panels show different mechanisms, not a required sequence. Solid arrows indicate loading; the dashed arrow indicates possible solute transport, not a measured flow vector. No depth, compass direction, duration or strain magnitude is assigned. Open full-size · Concept references: wiki.aapg.org · pressbooks.openeducationalberta.ca · doi.org
Conceptual section through a pumping well and observation piezometer: a curved potentiometric level stays above the confined aquifer roof, and the aquifer remains saturated. A separate calculation panel compares hydraulic diffusivities and times at a fixed Theis parameter. A separate added panel compares equal diffusivity with drawdowns 0.1451 m and 0.0725 m at fixed pumping rate, radius and time.
Confined head response and hydraulic diffusivity — Original GeoNavigate conceptual cross-section, not to spatial scale. The blue curve represents hydraulic head, not a drained rock boundary or a calculated drawdown profile. Up is toward the land surface; no compass direction or measured depth is assigned. Arrows indicate pumping and head decline. Numerical examples are invented and separate from the drawn geometry, not measured results or a reproduced publication figure. Added numerical panel: equal D does not fix drawdown magnitude; bars share a linear drawdown scale. Open full-size · Concept references: books.gw-project.org · books.gw-project.org · books.gw-project.org · pubs.usgs.gov
Two local sketches distinguish a stepped marker across discrete slip surfaces from a continuously sheared marker. A separate circular sector compares arc lengths at radii ten and twelve metres over sixty degrees.
Folding: localized slip, distributed shear and arc lengths — Original GeoNavigate conceptual illustration. Local shear sketches and layout are not to scale; arrows show relative motion only. The circular-sector geometry uses equal horizontal and vertical scales and invented dimensions. It is not a complete restored fold or a measured slip estimate. No compass direction, stratigraphic top, depth or elapsed time is implied. Open full-size · Concept references: psgt.earth.lsa.umich.edu · www.dal.ca · scholarsmine.mst.edu
Three time slices show facies belts advancing basinward across fixed position X. X records C, then B, then A; a separate column with an erosional gap lacks B.
Facies migration: time slices and a preserved vertical record — Original GeoNavigate conceptual illustration, not to scale. A, B and C are illustrative facies belts; horizontal rows are separate time snapshots, not beds or depth contours. Younging is upward in the columns. No compass direction, physical depth or duration is assigned. Open full-size · Concept references: geo.libretexts.org · geo.libretexts.org · www.geol.umd.edu
Upright conceptual sections compare horizontal beds onlapping a sloping lower surface, inclined beds downlapping a lower surface, and inclined beds ending beneath an upper toplap surface. Circles mark endpoints, not flow directions.
Reflection terminations: identify the bounding surface first — Original GeoNavigate conceptual cross-sections, not to scale. Thin lines represent selected strata; bold lines are bounding surfaces. No measured seismic trace, time or depth axis, compass bearing or numerical dip is implied. Baselap retains uncertainty between onlap and downlap. Open full-size · Concept references: sepmstrata.org · sepmstrata.org · people.wou.edu
Three comparable pelitic samples A, B and C lack garnet at A and contain garnet at B and C; a separate quartzite Q is not a valid garnet-absence control. A grain sketch shows a garnet relic with a later chlorite replacement patch.
Isograd evidence and a later mineral overprint — Original GeoNavigate conceptual observations, not to scale. Sample positions have no distance, depth or compass coordinate. The bracket constrains a possible garnet-in boundary only under the stated comparable-composition and preservation assumptions. The grain sketch illustrates a separate relative-timing observation, not a measured reaction or a pressure–temperature path. Open full-size · Concept references: www2.tulane.edu · www2.tulane.edu · pressbooks.lib.vt.edu
An invented pressure versus water saturation plot follows drainage leftward from full water saturation to a reversal at 0.20, then imbibition rightward. At water saturation 0.50 the paths have pressure differences of 8 and 4 kilopascals.
Same saturation, different displacement history — Original GeoNavigate conceptual illustration. Smooth paths are illustrative, not fitted data; marked coordinates are invented teaching values. Water is stipulated to be wetting, Pc = Pnonwetting minus Pwater. Arrows show displacement sequence, not spatial flow. No field pressure window or residual saturation calibration is implied. Open full-size · Concept references: mooseframework.inl.gov · glossary.slb.com · glossary.slb.com
A conceptual fixed-pressure solvus encloses a two-solid region. At the selected temperature the left phase contains 20 mass percent B, the right phase 80 percent, and the bulk contains 40 percent. The mass balance gives two-thirds left phase and one-third right phase.
Composition is not phase abundance — Original GeoNavigate conceptual diagram, not a published or calibrated mineral phase diagram. Temperature is qualitative and not to scale; the composition axis and mass-fraction bar use the stated invented values. The horizontal tie line joins equilibrium compositions, not positions in a rock. No spatial, depth or time scale. Open full-size · Concept references: www2.tulane.edu · www.southampton.ac.uk
Eight conceptual samples young upward from S1 to S8. Taxon A occurs from S2 to S6 and taxon B from S4 to S8; the common observed interval is S4 to S6. Dots mark sampled occurrences, while bars connect their limits.
Observed fossil ranges and their overlap — Original GeoNavigate conceptual illustration, not to scale. Sample ranks are evenly spaced for readability, not measured bed thickness or equal time. The section is stipulated upright and unrepeated; A and B are invented taxa. No measured depth, compass direction or numerical age is assigned. Open full-size · Concept references: stratigraphy.org · nacsn.americangeosciences.org
Hypothetical normalized isotope ratios place sample B at 0.980, sample A at 0.990 and the reference at 1.000. Their delta values are minus 20, minus 10 and zero per mil. A divided by B gives an isotope ratio factor of about 1.010204. A lower calculation distinguishes the 10 per mil delta difference from the 10.204 per mil relative ratio difference. A separate panel holds the sample fixed while changing the hypothetical reference ratio, producing delta values minus 10 and approximately minus 29.412 per mil.
Isotope delta: compare ratios on the same reference scale — Original GeoNavigate conceptual calculation with invented values. The horizontal axis is quantitative normalized isotope ratio, with a truncated range; it is not distance, depth or time. The diagram does not show a measured sample, reaction path or equilibrium calibration. The added comparison uses B as the denominator for the relative ratio difference; it is not a measured fractionation process. Lower reference-change panel is an algebra illustration, not a conversion between named isotope scales. Open full-size · Concept references: gml.noaa.gov · analyticalsciencejournals.onlinelibrary.wiley.com · web.mit.edu
Separate invented 100 kilogram systems each contain 1000 milligrams of a trace element. Partial melting partitions it into 600 milligrams in melt and 400 in residual solid. Crystal removal partitions it into 40 milligrams in removed crystals and 960 in remaining melt.
Melting and crystal removal: two separate mass balances — Original GeoNavigate conceptual accounting schematic, not to scale. Arrows indicate allocation of mass, not fluid paths, time, depth or compass direction. Values are invented; panels are separate systems, not successive stages or a measured magma chamber. Open full-size · Concept references: www2.tulane.edu · primer-computational-mathematics.github.io
Conceptual upright section with younger cover over a buried A, B and C soil profile. Root traces descend from the former surface. A separate bed has colour alone and remains an unconfirmed soil interpretation.
Buried soil versus a coloured sedimentary bed — Original GeoNavigate conceptual section, not to scale. No measured depths, age, climate or compass direction. A, B and C are simplified soil-horizon labels, not successive depositional ages. Open full-size · Concept references: www.usgs.gov · www.nrcs.usda.gov · www.usgs.gov
Upper aquifer head 104 metres and lower aquifer head 100 metres drive downward flow across a ten-metre aquitard. A separate calculation gives leakance and Darcy flux.
Head-driven leakage across an aquitard — Original GeoNavigate conceptual section, not to scale. Invented steady, one-dimensional, constant-density example; head values share a datum and are not layer elevations. Downward arrow indicates water flow, not drilling direction. No measured well or seal assessment. Open full-size · Concept references: www.usbr.gov · books.gw-project.org · www.usgs.gov
The same hypothetical cross-bed set upright and rotated 180 degrees. Its truncated original top is above in A and below in B; younging arrows reverse.
Cross-bed truncation and stratigraphic way-up — Original GeoNavigate conceptual sections, not to scale. B is A rotated 180 degrees; no measured dip, depth, current direction or fold geometry is implied. Arrows show younging, not drilling. Open full-size · Concept references: pressbooks.openeducationalberta.ca · serc.carleton.edu
Two hypothetical horizontal layers are each 1000 metres thick. At 2000 metres per second the upper layer contributes 1 second two-way time; at 4000 metres per second the lower contributes 0.5 seconds. The target is at 2000 metres and 1.5 seconds total two-way time.
Two layers: travel time and depth are different coordinates — Original GeoNavigate idealized vertical-ray example. Diagram not to spatial scale; time and depth columns have separate labelled scales. Common zero datum, downward-positive coordinates, no measured survey or regional velocity model. Open full-size · Concept references: www.eoas.ubc.ca · www.epa.gov · glossary.slb.com
Three conceptual rock faces distinguish layering without observed splitting, splitting parallel to bedding, and cleavage cutting bedding. All faces are arbitrarily oriented, without geographic or depth calibration.
Fissility, lamination and tectonic cleavage — Original GeoNavigate conceptual comparison, not to scale. Bands represent compositional layering; dark dashed lines represent splitting traces. Face orientation is arbitrary, not geographic horizontal. No measured sample or published figure is reproduced. Open full-size · Concept references: geology.arkansas.gov · pressbooks.openeducationalberta.ca · nora.nerc.ac.uk
A calcium carbonate formula connects to calcite and aragonite as distinct structures. Separate boxes distinguish chemical composition, current mineral identification and inherited external form.
Same composition, different mineral structures — Original GeoNavigate conceptual evidence diagram, not to scale. Boxes are labels, not unit cells or grain shapes. Connectors show shared composition, not a reaction, time sequence or pressure-temperature path. No measured data or publication figure. Open full-size · Concept references: www2.tulane.edu · www.nps.gov · sternberg.fhsu.edu
Two measuring points have elevations 110 and 105 metres; depths to water are 8 and 5 metres, giving heads 102 and 100 metres relative to one datum.
Water-level depth versus hydraulic head — Original conceptual measurement diagram, not to spatial scale. Invented values; downward arrows show tape depths, not groundwater flow. No aquifer geometry or water-table profile is inferred. Open full-size · Concept references: books.gw-project.org · books.gw-project.org
A conceptual serrated residue seam is compared with a visible open gap. Neither drawing predicts flow connectivity.
Stylolite seam versus open fracture — Original conceptual specimen-face drawings, not to scale. No geographic orientation, stress arrows, aperture measurement or flow prediction. Not reproduced publication figures. Open full-size · Concept references: glossary.slb.com
Two separate histories: older fossils redeposited in younger sediment, and fragments falling from an upper borehole wall into a deeper cuttings sample.
Fossil reworking and drilling cavings — Original conceptual comparison, not to scale. Drilling panel assumes an upright, unfaulted succession; depth increases downward. Arrows show transfer, not fluid velocity. No measured ages or well data. Open full-size · Concept references: stratigraphy.org · wiki.aapg.org
Two conceptual porcelain sections distinguish mineral powder lying on a plate from a groove cut into the plate.
Streak powder or scratched plate? — Original conceptual comparison, not to scale. Brown denotes hypothetical mineral powder, not a diagnostic mineral colour; grey denotes porcelain. No measured specimen or scratch depth. Open full-size · Concept references: msaweb.org · www.nps.gov
Three proportional bars compare a hypothetical gross interval of 20 metres, net reservoir of 12 metres and net pay of 8 metres. Their ratios to gross are 0.60 and 0.40.
Qualifying a net-to-gross ratio — Original hypothetical accounting example. Bar lengths are proportional to thickness totals, not a spatial log or measured reservoir. Net-reservoir and net-pay criteria differ; all quantities use the same thickness basis. References are linked in the worked guide. Open full-size
An upright column shows offshore mud passing upward into shoreface sand between lower and upper flooding surfaces; offshore mud overlies the upper surface. A bracket identifies the bounded package, not a maximum flooding surface.
Parasequence boundaries and evidence — Original GeoNavigate conceptual column: a shallowing-upward package lies between two flooding surfaces. Younging is upward; not to scale. No maximum flooding surface is assigned. Concept references: SEPM Strata and SLB Energy Glossary. Open full-size
Both specimens start straight and are held bent. After release the flexible specimen stays bent, while the elastic specimen returns straight.
Flexible versus elastic mineral behaviour — Original conceptual comparison, not to scale. Separate hypothetical specimens are shown before bending, while held bent and after release. Shapes are not force or strain measurements. Concept: MSA Mineral ID Key. Open full-size
Equal volumes of 0.0001 cubic metres contain 0.265 kilograms of sample or 0.100 kilograms of reference water; density ratio is 2.65 without units. A separate hydrostatic example shows air and submerged apparent weights of 2.65 and 1.65 newtons; their one-newton difference gives specific gravity 2.65.
Density and specific gravity: equal-volume comparison — Original hypothetical accounting schematic, not to spatial scale. Equal-sized boxes represent equal stipulated volumes, not crystal shapes. Reference water density is assumed to be 1000 kg/m³ for this example. Concepts: SLB density/specific gravity and Tulane mineral properties. Lower force bars share a 100-pixel-per-newton scale and are separate from the upper mass example. Open full-size · Concept references: www.gov.mb.ca
Total GR is one combined response; calibrated spectral processing estimates potassium in weight percent and uranium and thorium in ppm. These unlike units cannot simply be added.
Total GR and spectral components — Original GeoNavigate conceptual workflow, not to scale. Boxes describe outputs, not detector geometry, measured spectra or a published author figure. Open full-size · Concept references: glossary.slb.com · www.halliburton.com
Two static heads, 96 and 106 metres, lie above an aquifer roof at 80 metres; only the higher head exceeds the possible outlet at 101 metres.
Artesian head versus outlet elevation — Original GeoNavigate conceptual cross-sections, not to spatial scale. Independent invented cases with a common arbitrary elevation datum, positive upward. Tall tubes show static levels before opening an outlet; no flow rate is calculated. Open full-size · Concept references: books.gw-project.org
Two formula boxes hold calcium, silicon and oxygen constant while magnesium in diopside is replaced by ferrous iron in hedenbergite. A separate hypothetical ratio uses 0.6 magnesium and 0.4 ferrous iron.
Diopside and hedenbergite: ideal end-member chemistry — Original GeoNavigate conceptual composition schematic, not a crystal structure, phase diagram or measured sample. End-member formulas are idealized; real pyroxenes may contain other substitutions. Open full-size · Concept references: sites.und.edu · uwaterloo.ca
Calculated velocity follows 0.10 plus 0.60 sine of two pi t over eight seconds. It peaks at positive 0.70 metres per second and reaches negative 0.50, crossing zero despite a positive mean.
Combined flow: reversal with a mean current — Original calculated teaching plot; stipulated collinear velocities, not measured storm data. Axes are scaled; no spatial bedform geometry or sediment-transport prediction is implied. Open full-size · Concept references: doi.org · www.searchanddiscovery.com
Shallow measurement point z 90 metres has head 100 metres; deep point z 80 metres has head 102 metres. The head gradient is negative with elevation positive upward, and the assumed one-dimensional flow is upward.
Vertical gradient: screen elevation versus head — Original conceptual schematic, not to scale. Invented constant-density, one-dimensional example; separate points shown side by side for clarity, not to infer horizontal flow. Open full-size · Concept references: www3.epa.gov · books.gw-project.org
Water cap on a flat solid within oil. At the left contact, the interface tangent makes 60 degrees through water and 120 degrees through oil; both angles describe the same geometry.
One interface, two phase-side angles — Original conceptual cross-section, not to spatial scale. Circular-cap geometry has a 60-degree water-side tangent angle; no measured droplet, pore size or reservoir condition is represented. Open full-size · Concept references: glossary.slb.com · openpnm.org
Three conceptual sections compare an empty external mould, the same shape filled as a cast, and a smaller steinkern inside a dashed former shell outline.
Mould, cast or steinkern: which surface survives? — Original schematic sections, not to scale. Separate preservation outcomes, not a mandatory sequence. Smooth outlines omit shell ornament; the dashed line shows the former outer shell surface. Open full-size · Concept references: www.nps.gov · pressbooks.bccampus.ca
One cube of side two centimetres compared with eight separated cubes of side one centimetre; equal solid volume but twice the exposed surface area.
Breakage exposes more surface — Original idealized geometry, not to drawing scale. All six faces of every cube are exposed; no mass is lost and no reaction rate is measured. Open full-size · Concept references: slcc.pressbooks.pub
Upright section with taxon A at sample ranks 1 to 3 and taxon B at ranks 5 to 7. Highest occurrences at ranks 3 and 7 bound an interval; the two observed ranges do not overlap.
Interval boundaries without overlapping fossil ranges — Original GeoNavigate conceptual schematic, not to scale. Invented taxa and sample ranks; no measured thickness or numerical age. Dots are accepted occurrences, bars connect observed limits. Other fossils are stipulated in the intervening strata. Open full-size · Concept references: stratigraphy.org · nacsn.americangeosciences.org
Sodium plus silicon carry total charge plus five, equal to calcium plus aluminium. An ideal An30 composition has Na0.7 Ca0.3 Al1.3 Si2.7 O8, with cation charge plus sixteen balancing oxygen minus sixteen.
Plagioclase coupled substitution — Original GeoNavigate charge-accounting schematic; conceptual, not to scale. Boxes group chemical contributions, not crystal sites or atom sizes. Binary albite–anorthite model; no measured specimen. Open full-size · Concept references: www2.tulane.edu
Balanced pyrophyllite reaction produces one aluminium silicate, three quartz and one water per formula unit consumed. At one-quarter reaction progress, 0.75 mole pyrophyllite remains with 0.25 mole aluminium silicate, 0.75 mole quartz and 0.25 mole released water.
Metamorphic dehydration: balance and reaction progress — Original GeoNavigate conceptual accounting diagram, not to scale. Formula-unit and mole counts are stoichiometric, not mineral volumes. The aluminium-silicate polymorph depends on conditions; no temperature, pressure, reaction rate or fluid escape is inferred. Open full-size · Concept references: www2.tulane.edu · www2.tulane.edu
Two saturated streambed columns share stream head 100 metres. Lower head 100.2 metres gives upward Darcy flux 0.004 metres per day; lower head 99.8 metres gives equal downward flux.
Streambed seepage and head reversal — Original GeoNavigate conceptual sections, not to scale. Both columns stipulate steady one-dimensional saturated flow, uniform conductivity and equal-density water. Head values use one datum; arrows show seepage, not downstream channel flow. Open full-size · Concept references: pubs.usgs.gov · books.gw-project.org · books.gw-project.org
A cumulative mass-percent-finer plot has 30 percent at 0.125 mm and 70 percent at 0.25 mm. A straight segment on the logarithmic diameter axis crosses 50 percent at 0.177 mm.
Reading D50 from cumulative sieve masses — Original hypothetical calculation. Diameter uses a logarithmic axis; cumulative mass percent is linear. The dashed median construction assumes linear interpolation in log diameter between the two measured sieve points. No grain geometry or field sample is depicted. Open full-size · Concept references: www.fhwa.dot.gov · www.nhm.uio.no · apps.usgs.gov
Three independent conceptual sections: small crystals inside one host; plagioclase laths wholly inside a pyroxene host; and plagioclase laths crossing a pyroxene boundary in partial enclosure. A fourth panel distinguishes a large inclusion-free phenocryst in fine groundmass from the enclosure relationships above.
Crystal enclosure: poikilitic, ophitic and subophitic — Original conceptual two-dimensional sections, not to scale. Colours identify stipulated phases, not optical interference colours. Panels compare relationships and are not stages in a cooling sequence; mineral identities and host continuity are assumed for this exercise. The lower panel separates grain-size contrast from enclosure and does not prescribe a cooling history. Open full-size · Concept references: publications.iodp.org · www2.tulane.edu
Two equal-thickness layers with resistivities 10 and 90 ohm metres. Parallel current gives equivalent resistivity 18 ohm metres; perpendicular current gives 50 ohm metres. Separate ideal experiments, not a survey response.
Electrical resistivity along and across layers — Original conceptual sections, not to scale. Each layer is homogeneous and electrically isotropic; the stack is direction dependent. Arrows indicate conventional current direction only, not magnitude. Hypothetical DC boundary conditions; no well data. Open full-size · Concept references: www.eoas.ubc.ca
Five hypothetical samples ordered upward. Taxa A B and C are recorded together in S2 to S4, while A reaches 60 of 100 counted specimens only at S3. The evidence patterns differ; no formal zone boundaries are drawn.
Assemblage evidence versus abundance evidence — Original conceptual sample column, not to scale. Samples are ordered stratigraphically, not by elapsed time or measured depth. All counts are invented, with 100 identified specimens per sample. Presence dots and bars represent different evidence; no formal zone boundaries are assigned. Open full-size · Concept references: stratigraphy.org · nacsn.americangeosciences.org
Hypothetical upright sample ranks: A occurs at 1 to 5, B at 4 to 8 and C at 7 to 9. Independently stipulated succession A to B to C allows a candidate B lineage segment between lowest B at 4 and lowest C at 7, although B continues above 7.
A lineage segment is not necessarily a complete taxon range — Original conceptual sample-rank diagram, not to scale. Evolutionary succession is stipulated independently, not inferred from the plotted ranges. Lowest accepted occurrences are exercise inputs, not numerical ages or exact evolutionary origins. No real taxa or well samples. Open full-size · Concept references: stratigraphy.org · nacsn.americangeosciences.org
Five ordered sample positions. Positions 1 and 5 contain identified fossils, positions 2 and 4 were examined with none recovered, and position 3 was not sampled.
Sampled zero is different from no sample — Original conceptual sampling ledger, not to scale. Counts are invented and apply only to examined material. Blank sampling coverage is not a measured zero; neither establishes a hiatus. Open full-size · Concept references: stratigraphy.org
A conceptual saturated column contains an upper 10 metre layer with specific storage 0.00001 per metre and a lower 30 metre layer with 0.000003 per metre. Their storativity contributions are 0.00010 and 0.00009.
Thickness weighting in confined storage — Original hypothetical section, not to scale. Both layers remain confined and saturated. The common-decline calculation assumes the same 2 metre head decline in each layer, not drainage of a 2 metre thickness. Open full-size · Concept references: books.gw-project.org
Top and side orthographic views compare an ideal sphere of diameter 2 millimetres with an oblate spheroid measuring 2 by 2 by 0.4 millimetres. Both top views are circles, but the flattened grain has an elliptical side view.
A circular view can hide a flattened grain — Original ideal-shape construction. All four silhouettes use the same linear scale; these are projections, not thin-section cuts or measured grains. The short-to-long axis ratio is not presented as a sphericity index. Open full-size · Concept references: www.open.edu
Two profiles show a contact falling 10 metres over 100 metres horizontally. Equal scales show a 5.71 degree slope; fivefold vertical exaggeration shows 26.57 degrees. Depth increases downward.
Same section, two vertical scales — Original GeoNavigate numerical schematic, with axis scales specified: the upper plot uses 4 drawing units per metre on both axes; the lower uses 4 horizontally and 20 vertically. Hypothetical contact, not field data. Uniform resizing preserves each panel’s exaggeration; printed physical scale is not fixed. Open full-size · Concept references: pressbooks.bccampus.ca
Two radius-five-millimetre spheres touch. Their central section has touching circles, but a parallel section three millimetres away has radius-four circles separated by two millimetres.
A cut plane can miss a grain contact — Original GeoNavigate ideal geometry, not a measured rock or pore-network model. Both section panels use 30 drawing units per millimetre. Coordinates and plane offsets are stated; uniform resizing preserves proportions, not a fixed print scale. Open full-size · Concept references: publications.iodp.org
Three invented core-to-rim plagioclase profiles share axes. A decreases from An70 to An30, B increases from An30 to An70, and C alternates 70, 40, 60, 20, 30; A and C share endpoints but differ internally.
Plagioclase zoning: endpoints and internal variation — Original GeoNavigate schematic with exact plotted hypothetical values. Position is normalized from core to rim, not time or depth. Connecting lines guide the eye; no unmeasured profile is established. No physical crystal scale or natural sample is represented. Open full-size · Concept references: www2.tulane.edu · ntrs.nasa.gov · publications.iodp.org
Bulk D rises linearly from 0.2 to 4 as mineral B mass fraction rises from zero to one. D crosses one at B fraction 4/19, about 21.05 percent.
Bulk compatibility depends on mineral proportions — Original hypothetical calculation with fixed mineral coefficients 0.2 and 4. Axes are dimensionless, not time or depth. No named mineral or natural sample is represented. Open full-size · Concept references: primer-computational-mathematics.github.io
Two separate rock volumes have bulk volumes 100 and 300 cubic centimetres and pore volumes 10 and 90. Their combined porosity is 100 divided by 400, or 25 percent.
Porosity: add volumes before dividing — Original conceptual volume-accounting schematic, not to physical scale. Boxes are ledgers, not rock geometry or connected flow paths. Invented values. Open full-size · Concept references: books.gw-project.org
Conceptual bastite preserves one precursor outline; a separate mesh example divides one original grain domain into three cells. Cell count is not original grain count.
Bastite and mesh: inherited texture clues — Original GeoNavigate conceptual section, not to scale. Colours and short strokes are explanatory symbols, not optical colours or measured crystallographic orientations. No natural sample or publication artwork is reproduced. Open full-size · Concept references: publications.iodp.org · publications.iodp.org
Two hypothetical components with ages 10 and 30 million years yield a pooled apparent age of 23.22 million years, not their mean of 20.
Pooling isotope amounts versus averaging ages — Original GeoNavigate conceptual accounting schematic, not to spatial scale. Common proportional atom amounts; arrows add inventories at measurement. No geological event is assigned to the apparent age. Open full-size · Concept references: www.homepages.ucl.ac.uk
Twenty metres accumulate in two one-million-year intervals separated by a two-million-year pause. Whole-interval average is five, active average ten metres per million years.
Hiatus and average accumulation rate — Original quantitative hypothetical plot. Elapsed time increases forward; vertical axis is accumulated thickness, not borehole depth. Erosion and compaction are excluded. Open full-size · Concept references: www-odp.tamu.edu