Differential Subsidence
Differential Subsidence is a geomechanical phenomenon characterized by the uneven lowering of the Earth's surface due to spatially variable compaction of subsurface materials, distinguished from uniform subsidence by its heterogeneous magnitude and rate across adjacent regions.
119
Publications
5.1K
Citations
315
Authors
158
Institutions
Publications per year
2017–2026
16
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119
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158
Université Claude Bernard Lyon 1
Villeurbanne, France
4 h-index
4 publications
128 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
4 h-index
6 publications
401 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
19 publications
887 citations

Durham University
Durham, United Kingdom
4 h-index
6 publications
178 citations
Utrecht University
Utrecht, The Netherlands
3 h-index
9 publications
501 citations
Columbia University
New York, United States
3 h-index
6 publications
327 citations
United States Geological Survey
Reston, United States
3 h-index
7 publications
157 citations

University of the Basque Country
Leioa, Spain
2 h-index
8 publications
740 citations
1–8 of 158
11 publications · 502 citations
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JGR · 8 publications · 447 citations
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JGS · 7 publications · 611 citations
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6 publications · 243 citations
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4 publications · 95 citations
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