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  1. en.wikipedia.org › wiki › StratigraphyStratigraphy - Wikipedia

    Stratigraphy is a branch of geology concerned with the study of rock layers and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks . Stratigraphy has three related subfields: lithostratigraphy (lithologic stratigraphy), biostratigraphy (biologic stratigraphy), and chronostratigraphy ...

  2. Feb 21, 2023 · In geology and related studies, a stratum (plural strata) is defined as a sediment or rock layer with certain lithologic properties (texture, color, grain size, composition, etc.) distinctive from adjacent layers, separated by visible surface (bedding surface or plane).

  3. A thin lamina of clay deposited in the deep ocean, with slightly different composition and/or texture, caused by slight change in depositional conditions, that serves to distinguish it from underlying and overlying strata. A basalt flow spread over a land surface by a volcano.

  4. In lithostratigraphy, rock strata are placed in a hierarchy based upon several factors. Key among these is their lateral regional extent. The basic lithostratigraphic unit is called the formation. In order to be given this designation, a layer of rock must be mappable across an area.

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  5. May 29, 2018 · Stratigraphy is the study of rock layers (strata) deposited in the earth. It is one of the most challenging of geologic subdisciplines, comparable to an exacting form of detective work, yet it is also one of the most important branches of study in the geologic sciences.

  6. Mar 16, 2018 · Stratigraphy is a science that primarily deals with the study of layered sedimentary rocks (called strata) but may also include layered igneous rocks. Layered rocks may result from successive lava flows or from the formation of extrusive igneous rocks.

  7. Sequences of strata are genetically-related packages of rock bounded by unconformities. Within sequences, Walther’s Principle of facies migration apply. Across these sequence boundaries, it does not. Sediment needs its space: Accommodation, Sea Level, and Sediment supply. Basins are not static features.

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