Flexural Subsidence
Flexural Subsidence is a geodynamic process in which the lithosphere bends and sinks under the load of accumulating sediment or tectonic forces, resulting in regional subsidence along passive margins due to the elastic rheological response of the crust.
81
Publications
4.6K
Citations
240
Authors
123
Institutions
Publications per year
2017–2026
14
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1–5 of 81
240
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123
University of Oxford
Oxford, United Kingdom
4 h-index
7 publications
309 citations

Vrije Universiteit Amsterdam
Amsterdam, The Netherlands
4 h-index
13 publications
1.1K citations

University of Liverpool
Liverpool, United Kingdom
3 h-index
4 publications
332 citations
BP (United Kingdom)
London, United Kingdom
3 h-index
4 publications
160 citations
University of Arizona
Tucson, United States
3 h-index
5 publications
230 citations

Trinity College Dublin
Dublin, Ireland
2 h-index
3 publications
141 citations
United States Geological Survey
Reston, United States
2 h-index
3 publications
81 citations

University of Edinburgh
Edinburgh, United Kingdom
2 h-index
3 publications
91 citations
1–8 of 123
13 publications · 667 citations
13
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7 publications · 381 citations
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6 publications · 399 citations
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JGR · 6 publications · 464 citations
6
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JGS · 4 publications · 202 citations
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1–5