Postseismic Deformation
Postseismic Deformation is the time-dependent crustal deformation that occurs in the aftermath of an earthquake, distinguished from co-seismic and interseismic deformation by its occurrence subsequent to the main rupture and its primary control by relaxation processes such as afterslip, fault zone healing, and viscoelastic flow in the lower crust and upper mantle.
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The mechanics of earthquakes and faulting
Choice Reviews Online · 1990 · 3.6K citations
Coseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquake
Shinzaburo Ozawa, Takuya Nishimura, Hisashi Suito et al. · Nature · 2011 · 801 citations
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United States Geological Survey
Reston, United States
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183 publications
10.9K citations
California Institute of Technology
Pasadena, United States
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104 publications
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Centre National de la Recherche Scientifique
Paris, France
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213 publications
13.8K citations
University of California, Berkeley
Berkeley, United States
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75 publications
9K citations
Planetary Science Institute
Tucson, United States
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79 publications
8.2K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
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129 publications
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Tohoku University
Sendai, Japan
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145 publications
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Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
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JGR · 202 publications · 20.7K citations
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GJI · 110 publications · 5.8K citations
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BSSA · 73 publications · 4.6K citations
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