Bottom Current Sedimentation

Bottom Current Sedimentation is a sedimentary process within deep-sea environments characterized by the selective erosion, transport, and deposition of sediments by persistent near-bottom density-driven currents, distinguishing it from other deep-sea sedimentation mechanisms through its association with contour-following flow dynamics and formation of contourite deposits.

91

Publications

4K

Citations

325

Authors

166

Institutions

Publications per year

2017–2026

17

Variants

Contourite Sedimentation

Authors

325

  1. FJ
    F. Javier Hernández‐Molina

    Royal Holloway University of London, United Kingdom

    5 publications · 165 citations

    5

    h-index

  2. DV
    David Van Rooij

    Ghent University, Belgium

    4 publications · 142 citations

    4

    h-index

  3. EL
    Estefanía Llave

    Instituto Geológico y Minero de España, Spain

    4 publications · 145 citations

    4

    h-index

  4. AM
    Anxo Mena

    Universidade de Vigo, Spain

    3 publications · 100 citations

    3

    h-index

  5. TL
    Thomas Lüdmann

    Universität Hamburg, Germany

    3 publications · 218 citations

    3

    h-index

1–5 of 325

Venues

  1. Marine Geology

    24 publications · 985 citations

    18

    h-index

  2. Sedimentary Geology

    7 publications · 491 citations

    7

    h-index

  3. Sedimentology

    4 publications · 124 citations

    4

    h-index

  4. Geo-Marine Letters

    4 publications · 99 citations

    4

    h-index

  5. 3

    h-index

1–5