Bottom Current Processes

Bottom Current Processes is a sediment transport mechanism belonging to the class of deep-marine and lacustrine depositional processes, distinguished by the persistent movement of density-driven, near-bottom water flows that selectively erode, transport, and deposit fine-grained sediments along continental slopes and basin floors.

161

Publications

6.5K

Citations

499

Authors

222

Institutions

Publications per year

2017–2026

29

Authors

499

  1. FJ
    F. Javier Hernández‐Molina

    Royal Holloway University of London, United Kingdom

    10 publications · 597 citations

    10

    h-index

  2. MT
    Michael T. Ledbetter

    University of Georgia, United States

    6 publications · 235 citations

    6

    h-index

  3. MS
    Martyn S. Stoker

    British Geological Survey, United Kingdom

    6 publications · 352 citations

    6

    h-index

  4. MR
    Michele Rebesco

    National Institute of Oceanography and Applied Geophysics, Italy

    5 publications · 209 citations

    5

    h-index

  5. EL
    Estefanía Llave

    Instituto Geológico y Minero de España, Spain

    5 publications · 383 citations

    5

    h-index

1–5 of 499

Venues

  1. Marine Geology

    34 publications · 1.3K citations

    22

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 8 publications · 355 citations

    8

    h-index

  3. Sedimentary Geology

    6 publications · 263 citations

    6

    h-index

  4. 5

    h-index

  5. Sedimentology

    5 publications · 265 citations

    5

    h-index

1–5