Margin Subsidence
Margin Subsidence is a geological process denoting the gradual downward movement of the Earth's crust along continental margins, distinguished by lithospheric cooling, sediment loading, and tectonic forces that collectively drive vertical crustal deformation in passive or active margin settings.
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4.8K
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178
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99
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2017–2026
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Woods Hole Oceanographic Institution
Falmouth, United States
4 h-index
4 publications
312 citations

Imperial College London
London, United Kingdom
4 h-index
9 publications
277 citations

Scripps Institution of Oceanography
La Jolla, United States
3 h-index
4 publications
356 citations
Dalhousie University
Halifax, Canada
2 h-index
3 publications
380 citations
University College London
London, United Kingdom
2 h-index
5 publications
142 citations
Planetary Science Institute
Tucson, United States
2 h-index
2 publications
657 citations
Institute of Oceanology
Qingdao, China
2 h-index
3 publications
162 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
6 publications
104 citations
1–8 of 99
7 publications · 419 citations
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5 publications · 951 citations
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JGR · 5 publications · 505 citations
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4 publications · 229 citations
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JGS · 3 publications · 230 citations
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