Continental Rises

Continental Rises is a deep-sea geomorphic feature that constitutes the gently sloping sedimentary accumulation zone at the base of the continental slope, distinguishing itself from adjacent continental margins and abyssal plains by its transitional position and thick, graded deposits derived from turbidity currents and contourite processes.

155

Publications

12.2K

Citations

365

Authors

168

Institutions

Publications per year

2017–2026

6

Authors

365

  1. IN
    I Nick McCave

    University of Cambridge, United Kingdom

    5 publications · 150 citations

    5

    h-index

  2. BE
    Brian E. Tucholke

    Woods Hole Oceanographic Institution, United States

    4 publications · 107 citations

    4

    h-index

  3. JL
    J. Lamar Worzel

    Lamont-Doherty Earth Observatory, United States

    4 publications · 144 citations

    4

    h-index

  4. BC
    Bruce C. Heezen

    Lamont-Doherty Earth Observatory, United States

    4 publications · 634 citations

    4

    h-index

  5. CD
    Charles D. Hollister

    Woods Hole Oceanographic Institution, United States

    4 publications · 637 citations

    4

    h-index

1–5 of 365

Venues

  1. Geological Society of America Bulletin

    14 publications · 2.7K citations

    14

    h-index

  2. AAPG Bulletin

    15 publications · 1K citations

    14

    h-index

  3. Marine Geology

    14 publications · 494 citations

    13

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 9 publications · 2.4K citations

    9

    h-index

  5. Geological Society London Special Publications

    8 publications · 368 citations

    8

    h-index

1–5