Half-graben Geometry

Half-Graben Geometry is a structural tectonic construct characterized by a depressed crustal block bounded by a single major normal fault on one side and a flexural hinge or minor fault system on the opposite side, distinguishing it from symmetric graben structures through its asymmetric cross-sectional form.

90

Publications

4.2K

Citations

266

Authors

123

Institutions

Publications per year

2017–2026

11

Authors

266

  1. KM
    Ken McClay

    Royal Holloway University of London, United Kingdom

    3 publications · 127 citations

    3

    h-index

  2. AR
    Alan Roberts

    University of Liverpool, United Kingdom

    3 publications · 125 citations

    3

    h-index

  3. BJ
    B. J. Drummond

    Geological Survey of Western Australia, Australia

    2 publications · 52 citations

    2

    h-index

  4. GY
    G. Yielding

    University of Liverpool, United Kingdom

    2 publications · 106 citations

    2

    h-index

  5. LE
    Lynne E. Frostick

    University of Hull, United Kingdom

    2 publications · 93 citations

    2

    h-index

1–5 of 266

Venues

  1. Geological Society London Special Publications

    17 publications · 1.1K citations

    16

    h-index

  2. Journal of Structural Geology

    6 publications · 269 citations

    6

    h-index

  3. Geological Society London Petroleum Geology Conference series

    Conference · 4 publications · 211 citations

    4

    h-index

  4. Journal of the Geological Society

    JGS · 4 publications · 475 citations

    4

    h-index

  5. Sedimentary Geology

    3 publications · 61 citations

    3

    h-index

1–5