Basin Subsidence
Basin Subsidence is a geological process denoting the downward vertical displacement of a sedimentary basin’s lithospheric crust in response to tectonic, sedimentary, or magmatic loading, distinguished within the context of lithospheric flexure and planetary isostasy by its reliance on the flexural rigidity of the lithosphere and isostatic compensation mechanisms to explain the temporal and spatial evolution of subsidence.
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Sedimentary basins: evolution, facies, and sediment budget
Gerhard Einsele · Choice Reviews Online · 1992 · 781 citations
Christopher Beaumont · Geophysical Journal International · 1981 · 731 citations · Full text
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Centre National de la Recherche Scientifique
Paris, France
32 h-index
125 publications
6.2K citations

Chinese Academy of Sciences
Beijing, China
26 h-index
154 publications
8.5K citations
United States Geological Survey
Reston, United States
26 h-index
67 publications
3.7K citations

Vrije Universiteit Amsterdam
Amsterdam, The Netherlands
25 h-index
68 publications
5K citations
The University of Texas at Austin
Austin, United States
21 h-index
55 publications
2.2K citations

China University of Geosciences (Beijing)
Beijing, China
21 h-index
74 publications
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Sorbonne Université
Paris, France
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37 publications
1.9K citations
Universitat de Barcelona
Barcelona, Spain
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44 publications
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