Gravity-driven Sedimentation

Gravity-Driven Sedimentation is a geological process in which slope sediments are transported and deposited under the influence of gravitational forces, distinguished from other sedimentation mechanisms by its primary reliance on gravity-induced downslope movement such as landslides, debris flows, and turbidity currents.

68

Publications

2.8K

Citations

228

Authors

101

Institutions

Publications per year

2017–2026

16

Authors

228

  1. AC
    A. C. Leopold

    Purdue University West Lafayette, United States

    2 publications · 75 citations

    2

    h-index

  2. AA
    AA Axelrad

    University of Toronto, Canada

    2 publications · 167 citations

    2

    h-index

  3. RP
    Robert Peter Gale

    Imperial College London, United Kingdom

    2 publications · 67 citations

    2

    h-index

  4. MM
    M. Mitsu Suyemoto

    North Carolina State University, United States

    2 publications · 75 citations

    2

    h-index

  5. JF
    John F. Hiemstra

    Swansea University, United Kingdom

    2 publications · 40 citations

    2

    h-index

1–5 of 228

Venues

  1. Marine and Petroleum Geology

    6 publications · 201 citations

    6

    h-index

  2. Marine Geology

    4 publications · 147 citations

    4

    h-index

  3. American Journal of Botany

    3 publications · 95 citations

    3

    h-index

  4. Science China Earth Sciences

    2 publications · 29 citations

    2

    h-index

  5. Blood

    2 publications · 167 citations

    2

    h-index

1–5