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

Authors

8K

  1. RB
    Roland Bürgmann

    University of California, Berkeley, United States

    66 publications · 4.8K citations

    41

    h-index

  2. JA
    Jean‐Philippe Avouac

    California Institute of Technology, United States

    43 publications · 7.2K citations

    37

    h-index

  3. YK
    Yann Klinger

    Institut de physique du globe de Paris, France

    28 publications · 3.4K citations

    26

    h-index

  4. XX
    Xiwei Xu

    China Earthquake Administration, China

    36 publications · 2.6K citations

    24

    h-index

  5. PB
    Pierre Briole

    Centre National de la Recherche Scientifique, France

    29 publications · 1.8K citations

    23

    h-index

1–5 of 8K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 338 publications · 35.7K citations

    102

    h-index

  2. Geophysical Research Letters

    353 publications · 23.7K citations

    83

    h-index

  3. Tectonophysics

    280 publications · 12.8K citations

    62

    h-index

  4. Geophysical Journal International

    GJI · 211 publications · 10.9K citations

    59

    h-index

  5. Bulletin of the Seismological Society of America

    BSSA · 197 publications · 12.7K citations

    58

    h-index

1–5