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67:. Academic geologists study subterranean basins as well as those basins which have been exhumed and dissected by subsequent tectonic events. Thus academics sometimes use petroleum industry techniques, but in many cases they are able to study rocks at the surface. Techniques used to study surficial sedimentary rocks include: measuring stratigraphic sections, identifying
35:. Subsidence of sedimentary basins generates the spatial distribution of accommodation infilling sediments. Aspects of the sediment, namely its composition, primary structures, and internal architecture, can be synthesized into a history of the basin fill. Such a synthesis can reveal how the basin formed, how the sediment fill was
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or precipitated, and reveal sources of the sediment fill. From such syntheses models can be developed to explain broad basin formation mechanisms. Examples of such basin classifications include intracratonic, rift, passive margin, strike-slip, forearc, backarc-marginal sea, fold and thrust belt, and
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Lee, E.Y., Novotny, J., Wagreich, M., Subsidence analysis and visualization: for sedimentary basin analysis and modelling, Springer, (2019).
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and hydrocarbon-bearing rocks in a basin, and the academic geologist, who may be concerned with any or all facets of a basin's evolution.
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Duppenbecker S. J. and Eliffe J. E., Basin
Modelling: Practice and Progress, Geological Society Special Publication, (1998).
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Evenick, J. C., Glimpses into Earth's history using a revised global sedimentary basin map, Earth-Science
Reviews, (2021).
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basin analysis is often conducted on subterranean basins through the use of
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Lerche I., Basin
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