Low-angle Faults

Low-Angle Faults is a structural geological construct denoting a fracture or shear zone in the Earth's crust where the dip angle relative to the horizontal is less than 30 degrees, distinguished from high-angle faults by its shallow inclination and commonly associated with large-scale crustal extension or compression in marine tectonic settings.

286

Publications

20.9K

Citations

790

Authors

295

Institutions

Publications per year

2017–2026

37

Variants

Low-angle Fault

Authors

790

  1. CC
    Cristiano Collettini

    Istituto Nazionale di Geofisica e Vulcanologia, Italy

    9 publications · 1K citations

    9

    h-index

  2. MP
    M. P. Searle

    University of Oxford, United Kingdom

    7 publications · 1.4K citations

    7

    h-index

  3. WR
    W. Roger Buck

    Lamont-Doherty Earth Observatory, United States

    5 publications · 1.1K citations

    5

    h-index

  4. PB
    Pierre Briole

    Centre National de la Recherche Scientifique, France

    5 publications · 351 citations

    5

    h-index

  5. MR
    Massimiliano Rinaldo Barchi

    University of Perugia, Italy

    5 publications · 382 citations

    5

    h-index

1–5 of 790

Venues

  1. Geology

    26 publications · 2.9K citations

    23

    h-index

  2. Geological Society London Special Publications

    23 publications · 1.5K citations

    19

    h-index

  3. Journal of the Geological Society

    JGS · 22 publications · 1.8K citations

    18

    h-index

  4. Tectonics

    19 publications · 1.7K citations

    17

    h-index

  5. Geological Society of America Bulletin

    16 publications · 1.1K citations

    15

    h-index

1–5