Listric Fault Geometry

Listric Fault Geometry is a structural geological model characterized by a concave-upward, curvilinear fault surface that dips steeply at shallow depths and shallows with increasing depth, distinguishing it from planar or other non-curved fault geometries in extensional tectonic settings.

188

Publications

10.6K

Citations

517

Authors

226

Institutions

Publications per year

2017–2026

17

Authors

517

  1. KM
    Ken McClay

    Royal Holloway University of London, United Kingdom

    5 publications · 474 citations

    5

    h-index

  2. MP
    M. P. Coward

    University of Leeds, United Kingdom

    3 publications · 233 citations

    3

    h-index

  3. CE
    C. E. Willman

    Geological Survey of Western Australia, Australia

    3 publications · 216 citations

    3

    h-index

  4. PJ
    P. J. O'Shea

    Geoscience Australia, Australia

    3 publications · 216 citations

    3

    h-index

  5. SM
    Shankar Mitra

    University of Oklahoma, United States

    3 publications · 162 citations

    3

    h-index

1–5 of 517

Venues

  1. Geological Society London Special Publications

    23 publications · 1.3K citations

    18

    h-index

  2. AAPG Bulletin

    24 publications · 2.2K citations

    18

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 18 publications · 1.7K citations

    17

    h-index

  4. Journal of Structural Geology

    11 publications · 576 citations

    11

    h-index

  5. Basin Research

    11 publications · 499 citations

    11

    h-index

1–5