Coseismic Deformation
Coseismic Deformation is a form of crustal deformation that consists of the instantaneous to very rapid displacement and strain of the Earth’s surface and subsurface that occurs contemporaneously with an earthquake rupture and is directly caused by slip on the causative fault.
3.6K
Publications
207K
Citations
8K
Authors
1.5K
Institutions
Publications per year
2017–2026
930
8K
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California Institute of Technology, United States
43 publications · 7.2K citations
37
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26
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24
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23
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1.5K
United States Geological Survey
Reston, United States
68 h-index
421 publications
26.2K citations

Centre National de la Recherche Scientifique
Paris, France
66 h-index
609 publications
38.9K citations
California Institute of Technology
Pasadena, United States
64 h-index
307 publications
49.6K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
62 h-index
1.1K publications
69.2K citations

Institut de physique du globe de Paris
Paris, France
58 h-index
274 publications
25.2K citations
Planetary Science Institute
Tucson, United States
50 h-index
160 publications
14.6K citations
China Earthquake Administration
Beijing, China
49 h-index
818 publications
37.5K citations
The University of Tokyo
Tokyo, Japan
49 h-index
245 publications
15.9K citations
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JGR · 338 publications · 35.7K citations
102
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353 publications · 23.7K citations
83
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280 publications · 12.8K citations
62
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GJI · 211 publications · 10.9K citations
59
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BSSA · 197 publications · 12.7K citations
58
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