Fault-block Mountains

Fault-Block Mountains is a type of mountain landform characterized by large-scale uplifted or down-dropped crustal blocks bounded by normal or reverse faults, resulting from tectonic extension or compression that fractures and displaces rigid segments of the Earth's lithosphere.

61

Publications

3.2K

Citations

174

Authors

72

Institutions

Publications per year

2017–2026

5

Variants

Fault-block Mountain

Authors

174

  1. JZ
    Jin Zhang

    Chinese Academy of Geological Sciences, China

    2 publications · 65 citations

    2

    h-index

  2. JH
    Jonny Hesthammer

    Equinor (Norway), Norway

    2 publications · 29 citations

    2

    h-index

  3. DC
    Dickson Cunningham

    University of Leicester, United Kingdom

    2 publications · 65 citations

    2

    h-index

  4. DF
    Daniel F. Stöckli

    The University of Texas at Austin, United States

    2 publications · 209 citations

    2

    h-index

  5. AM
    André Michard

    University of Hassan II Casablanca, Morocco

    2 publications · 169 citations

    2

    h-index

1–5 of 174

Venues

  1. The Journal of Geology

    JG · 7 publications · 146 citations

    7

    h-index

  2. Marine and Petroleum Geology

    3 publications · 107 citations

    3

    h-index

  3. AAPG Bulletin

    3 publications · 48 citations

    3

    h-index

  4. Geological Society of America Bulletin

    3 publications · 59 citations

    3

    h-index

  5. Journal of Asian Earth Sciences

    3 publications · 65 citations

    3

    h-index

1–5