High-density Turbidity Currents

High-Density Turbidity Currents is a type of sediment gravity flow characterized by high sediment concentration and turbulent fluid support, distinguished from low-density counterparts by its ability to generate grain-to-grain interactions and sustained turbulent suspension, resulting in massive to normally graded bedding with distinctive erosional and depositional structures in deep-marine environments.

102

Publications

9.8K

Citations

241

Authors

138

Institutions

Publications per year

2017–2026

12

Authors

241

  1. MC
    Matthieu Cartigny

    Durham University, United Kingdom

    2 publications · 170 citations

    2

    h-index

  2. DR
    Donald R. Lowe

    Stanford University, United States

    2 publications · 2.7K citations

    2

    h-index

  3. LA
    Luís A. Buatois

    University of Saskatchewan, Canada

    2 publications · 81 citations

    2

    h-index

  4. MJ
    Michael J. Benton

    University of Bristol, United Kingdom

    2 publications · 68 citations

    2

    h-index

  5. JI
    Jasim Imran

    University of South Carolina, United States

    2 publications · 395 citations

    2

    h-index

1–5 of 241

Venues

  1. Journal of Sedimentary Research

    JSR · 14 publications · 3.5K citations

    14

    h-index

  2. Sedimentology

    8 publications · 1.2K citations

    8

    h-index

  3. AAPG Bulletin

    7 publications · 488 citations

    7

    h-index

  4. Sedimentary Geology

    5 publications · 197 citations

    5

    h-index

  5. Geo-Marine Letters

    4 publications · 195 citations

    4

    h-index

1–5