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.

1.2K

Publications

82.5K

Citations

2.8K

Authors

806

Institutions

Publications per year

2017–2026

261

Authors

2.8K

  1. RB
    Roland Bürgmann

    University of California, Berkeley, United States

    45 publications · 3.8K citations

    31

    h-index

  2. FF
    Fred F. Pollitz

    United States Geological Survey, United States

    37 publications · 3.2K citations

    29

    h-index

  3. JC
    J. C. Savage

    United States Geological Survey, United States

    29 publications · 3.3K citations

    19

    h-index

  4. WT
    Wayne Thatcher

    United States Geological Survey, United States

    21 publications · 2.2K citations

    19

    h-index

  5. JT
    Jeffrey T. Freymueller

    University of Alaska Fairbanks, United States

    19 publications · 1.4K citations

    17

    h-index

1–5 of 2.8K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 202 publications · 20.7K citations

    85

    h-index

  2. Geophysical Research Letters

    142 publications · 7K citations

    52

    h-index

  3. Geophysical Journal International

    GJI · 110 publications · 5.8K citations

    41

    h-index

  4. Journal of Geophysical Research Solid Earth

    96 publications · 4K citations

    37

    h-index

  5. Bulletin of the Seismological Society of America

    BSSA · 73 publications · 4.6K citations

    36

    h-index

1–5