Isostatic Equilibrium
Isostatic Equilibrium is a geophysical state in which the Earth's lithosphere achieves static balance over the asthenosphere due to buoyant forces counteracting surface load changes, such that vertical crustal motions cease in response to glacial or oceanic mass redistribution.
180
Publications
11.8K
Citations
376
Authors
198
Institutions
Publications per year
2017–2026
17
Variants
Isostasy
Parents
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198

Centre National de la Recherche Scientifique
Paris, France
6 h-index
12 publications
1.4K citations
Utrecht University
Utrecht, The Netherlands
6 h-index
15 publications
714 citations

Delft University of Technology
Delft, The Netherlands
5 h-index
7 publications
309 citations
University of Cambridge
Cambridge, United Kingdom
5 h-index
7 publications
578 citations

Cornell University
Ithaca, United States
4 h-index
6 publications
364 citations
Massachusetts Institute of Technology
Cambridge, United States
4 h-index
7 publications
306 citations

Christian-Albrechts-Universität zu Kiel
Kiel, Germany
4 h-index
8 publications
279 citations
Planetary Science Institute
Tucson, United States
4 h-index
5 publications
260 citations
1–8 of 198
JGR · 33 publications · 2.3K citations
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GJI · 23 publications · 1K citations
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12 publications · 922 citations
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6 publications · 158 citations
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PRL · 6 publications · 387 citations
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