Bottom Current Deposits

Bottom Current Deposits is a type of deep-marine sedimentary deposit characterized by its formation from the reworking and accumulation of sediments transported and winnowed by persistent bottom-intensified ocean currents, distinguishing it from deposits primarily formed by turbidity flows or pelagic settling.

99

Publications

4.1K

Citations

291

Authors

149

Institutions

Publications per year

2017–2026

14

Authors

291

  1. FT
    Fabio Trincardi

    Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche, Italy

    5 publications · 287 citations

    5

    h-index

  2. GS
    G. Shanmugam

    The University of Texas at Arlington, United States

    5 publications · 323 citations

    5

    h-index

  3. GE
    Gemma Ercilla

    Institut de Ciències del Mar, Spain

    4 publications · 150 citations

    4

    h-index

  4. FJ
    F. Javier Hernández‐Molina

    Royal Holloway University of London, United Kingdom

    4 publications · 151 citations

    4

    h-index

  5. AR
    Adriano R. Viana

    Petrobras (Brazil), Brazil

    3 publications · 140 citations

    3

    h-index

1–5 of 291

Venues

  1. Marine Geology

    19 publications · 566 citations

    15

    h-index

  2. Geological Society London Special Publications

    7 publications · 273 citations

    7

    h-index

  3. Sedimentary Geology

    5 publications · 209 citations

    5

    h-index

  4. Sedimentology

    4 publications · 254 citations

    4

    h-index

  5. AAPG Bulletin

    4 publications · 351 citations

    4

    h-index

1–5