Thrust Faulting

Thrust faulting is a type of brittle deformation characterized by the low-angle reverse movement of rock masses along a fault plane, in which the hanging wall moves upward over the footwall due to compressional stresses, typically occurring within the context of continental collision, lithospheric deformation, mountain building, and Quaternary tectonics.

496

Publications

29.8K

Citations

1.3K

Authors

475

Institutions

Publications per year

2017–2026

59

Authors

1.3K

  1. PM
    Péter Molnár

    Massachusetts Institute of Technology, United States

    12 publications · 3.4K citations

    12

    h-index

  2. TR
    T. R. Watters

    Smithsonian Institution, United States

    7 publications · 852 citations

    7

    h-index

  3. JB
    John B. Rundle

    University of California, Davis, United States

    6 publications · 320 citations

    6

    h-index

  4. ET
    Enrico Tavarnelli

    University of Siena, Italy

    5 publications · 184 citations

    5

    h-index

  5. PL
    Pierre Labaume

    Université de Montpellier, France

    5 publications · 185 citations

    5

    h-index

1–5 of 1.3K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 58 publications · 7.7K citations

    40

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  2. Tectonics

    39 publications · 2.7K citations

    28

    h-index

  3. Journal of Structural Geology

    30 publications · 1.7K citations

    23

    h-index

  4. Geophysical Journal International

    GJI · 27 publications · 1.3K citations

    22

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  5. Geophysical Research Letters

    24 publications · 1.4K citations

    21

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1–5