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Sequence stratigraphic principles

Eocene Shelf parasequences, Ellesmere Island

The focus in this series of the Virtual Classroom is Sequence Stratigraphy.  Four introductory posts will look briefly at the history of stratigraphic concepts (timelines) from the 15th century to 1977, and the development of chronostratigraphy. Subsequent posts will outline some of the underpinning foundations of sequence stratigraphy (and genetic stratigraphy in general), for example, base level, sea level fluctuations, cycles and parasequences, stacking patterns, shoreline trajectories, clinoforms, sediment accommodation, and supply, sedimentary facies and facies models, condensed sections, systems tracts, and a brief look at the different sequence stratigraphic models.

A timeline of stratigraphic principles; 15th to 18th C

A timeline of stratigraphic principles; 19th C to 1950

A timeline of stratigraphic principles; 1950-1977

All the stratigraphies

Baselevel, Base-level, and Base level

Sediment accommodation and supply

Facies and facies models

How to read a sea level curve

Autogenic or allogenic dynamics in stratigraphy?

Stratigraphic cycles: What are they?

Sequence stratigraphic surfaces

Parasequences

Shorelines and shoreline trajectories

Stratigraphic trends and stacking patterns

Clinoforms and clinothems

Stratigraphic lapouts

sequence stratigraphic

Stratigraphic condensation – condensed sections

Depositional systems and systems tracts

An idealised panorama of depositional systems across terrestrial and marine environments.

Which sequence stratigraphic model is that?

Beach microcosms as fan delta analogues

Stratigraphic surfaces in outcrop – baselevel fall

Stratigraphic surfaces in outcrop – baselevel rise

Archives
Categories
dip and strike compass
Measuring dip and strike
sandstone classification header
Classification of sandstones
Calcite cemented subarkose, Proterozoic Altyn Fm. southern Alberta
Sandstones in thin section
poles to bedding great circles
Stereographic projection – poles to planes
froude-reynolds-antidunes-header-768x439-1
Fluid flow: Froude and Reynolds numbers
Stokes Law for particle settling in a schematic context of other fluid flow functions
Fluid flow: Stokes Law and particle settling
sedimentary-basins-distribution-1-768x711
Classification of sedimentary basins
Model are representational descriptions are written in different languages - diagrammatic, descriptive, mathematical, and conceptual. They commonly contain variables and dimensionless quantities that permit quantitative analysis of the physical systems the models represent.
Geological models
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