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Sequence Stratigraphy Terminology

Accommodation
Aggradation
Aggradational Parasequence Set
Allostratigraphy
Allocyclic
Allogenetic
Architectural Elements
Autocyclic
Autogenetic
Basal Surface Forced Regression
Baselap
Base level
Basin
Basin-floor Fan
Basinward Shift in Facies
Bayline
Bed
Bedding Plane
Bedset
Biostratigraphy
Biozone
Boundaries
Bounding Surfaces

Carbonate
Chronostratigraphic Correlation Chart
Chronostratigraphy
Clinoform Surface
Coastal Offlap
Coastal Onlap
Coastal Plain
Coastal Trajectory
Composite Sequence
Concordance
Condensed Section
Conformity
Corelative conformity

Cycles and rhythms
Cycles: 1st order, 2nd order, 3rd order, 4th order, 5th order
Deepening Upward Cycle
Deepwater Fans
Deepwater Sediments
Deltaic Plain
Deltaic Plume
Density Log
Depostional Elements

Depositional-shoreline Break

Depositional Sequence
Depositional Surface
Depositional System
Diachrone
Diachronous
Disconformity
Discordance
Distal-Fan
Dolomite
Downlap
Downlap Surface
Drowning Surface
Early Lowstand System Tract
Ecological Accomodation
Equilibrium Point
Erosional Truncation
Eustasy
Eustatic Inflection points
Eutrophic
Events
Facies Tracts
Facies Trajectory
Falling Stage System Tract
Firm Grounds
Flooding Surface
Fondoform Surface
Formation
Forced Regression
Gamma Log
Genetic Sequence
Glauconite
Glossifungites
Hemipelagic sediments
Hiatus
Hierarchial Boundaries
Hierarchial Elements

High-frequency cycle "cycle"
High-Frequency Sequences (HFS)
Highstand System Tract
Hinterland Sequence
Homopycnal Flow
Hyperpycnal Flow
Hypopycnal Flow
Incised Valley
Inchnofacies
Inchnofossils
Inter-regional Unconformity
Intraclasts
Isochrone
Lamina
Laminaset
Lapout
Late Lowstand System Tract
Law of Faunal Succession
Law of Lateral Continuity
Law of Original Horizontallity
Law of Stratigraphic Succession (Superposition)
Limestone
Lithofacies
Lithology
Lithostratigraphy
Lowstand System Tract
Lowstand Wedge
Magnetostratigraphy
Marine Flooding Surface
Maritime Sequence
Maximum Flooding Surface (MFS)
Maximum Regressive Surface (MRS)
Measurement of Eustasy
Mesotrophic
Micrite
Mid-Fan
Mid-Slope-Channels
Milankovitch Cycles
Mound Seismic Reflection Configuration
Neutron Log
Normal Regression
Nutrients
Offlap
Offlapping Coast
Oligotrophic
Onlap
Oolites
Parasequence Set
Parasequence
Parasequence - Clastic Beach
Parasequence - Clastic Shore
Parasequence - Delta
Parasequence - Stacked Beaches
Parasequence - Tidal Falt
Pelagic sediments
Pellets
Physical Accomodation
Prograding lowstand
Progradation
Progradational Parasequence Set
Proximal-Fan
Size of Eustatic Excursions
Radiometric Dating
Ramp to Rim Carbonate
Ravinement Erosion Surface

Regression
Regressive Surface of Erosion
Regressive System Tract
Relative Sea Level
Relative Sea Level Fall
Relative Sea Level Rise
Resistivity Logs
Retrogradation
Retrogradational Parasequence Set
Rhythms and Cycles
Sedimentary Structures

Sedimentary Supply
Sequence
Sequence Stratigraphic Models
Sequence Boundary
Sequence Stratigraphy
Shelf Break
Shelf-margin System Tract
Shelf Margin Trajectory
Shoreline
Shoreline Trajectory
Sigmoid Configuration
Size of Sea Level Excursions

Seismic Sequence
Skeletal Grains
Slope Fan
Sonic (acoustic) Log
Spontaneous Potential (SP)
Log
Stacking Patterns
Stratigraphic Surfaces
Stratigraphy
Stratum (strata)
Supercycle
Surfaces
Systems Tract
Tempestite
Terminations
Tiering of Trace Fossils
Toe-of-Slope-Fan
Topset

Toplap
Trace Fossils
Trajectory of Shoreline
Transgression
Transgressive Lag
Transgressive System Tract
Transgressive Surface
Transgressive-Regressive Sequence
Truncation
Type 1 Sequence Boundary

Type 2 Sequence Boundary
Turbidite
Unconformity
Undaform Surface
Uniformitarianism
Vertical Facies Successions (VFS)
Wave Base
Walther's Law of Correlation of Facies
Wheeler diagram

Introduction
This "listing" of the terminology used by sequence stratigraphers has been under constant development since we began this site and the list is likely to remain incomplete. Compilation reflects our personal interests, experience and the inadequate time we are able to devote to building it. Sometimes what we have produced is incorrect, poorly written or illustrated. Please let us know if you find anything that you think is wrong or could be improved and we will try to correct our errors. If you have something that you think should be changed or could be added, please mail this to us with text and .jpg or .gif illustrations and we will put place these on the site and acknowledge your contribution. We welcome your help. This is our site but it is yours too!

We refer you to the debate on the Formalization of Sequence Stratigraphy methodology, surfaces, units and terminology launched by Octavian Catuneanu and Ashton Embry through the IWGSS (International Working Group on Sequence Stratigraphy) and the International Sub-commission on Stratigraphic Classification (ISSC) Task Group on Sequence Stratigraphy. Comments are posted for these groups so their manuscripts can be revised. As you can see differences in opinion exist. These are a reflection of a healthy difference in our understanding of this evolving science.

Philosophy on the use of terms
Krynine is alleged to have said that "stratigraphy is the triumph of terminology over common sense". At one time or another, anyone who has had anything to do with sequence stratigraphy has probably sympathized with Krynine's position. The science of sequence stratigraphy is replete with jargon. The "standardized" terminology listed and defined below, can be intimidating to learn. However it offers powerful tools for describing surfaces, strata, terminations, and other abstract concepts that are key to understanding the evolution of stratigraphic architecture.

Our personal advice to the users of sequence stratigraphy is that they concentrate on understanding the principles of this topic and how to use them. Never the less stratigraphy changes as do the models that explain what we see in the rock record. If our "current" terminology does not fit a particular configuration of the rocks being examined, then we should carefully define and describe this configuration, using terms we believe meet the needs of the situation, and move on. Purists may be disturbed by our usage, but so long as we have carefully defined what we mean, others really should have no quarrel with us. Science evolves and changes and we should accommodate our language to meet these changes. Most people who are advocating changes to the list below are serious scientists with genuine arguments against some of the current usage within specific geological settings.

In other words, use the terminology that suits you best but define this terminology as carefully as you can, preferably using colloquial language. At the same time we do not to advocate arbitrarily changing terms to give them a personalized gee-whiz pizzazz, anymore than we would argue for Humpty Dumpty's position from Lewis Carroll’s Through the Looking Glass: "When I use a word, it means just what I choose it to mean - nothing more nor less".

 

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Last Revised: December 27, 2007