Glacial-driven Turbidity Currents

Glacial-Driven Turbidity Currents is a type of sediment gravity flow initiated by the sudden release of glacially derived sediments into marine environments, distinguished by its direct linkage to glacial processes such as iceberg calving, meltwater discharge, or subglacial sediment-laden outburst floods.

22

Publications

1.4K

Citations

86

Authors

40

Institutions

Publications per year

2017–2026

7

Authors

86

  1. AN
    Alexandre Normandeau

    Geological Survey of Canada, Canada

    3 publications · 78 citations

    3

    h-index

  2. CÓ
    Colm Ó Cofaigh

    Durham University, United Kingdom

    2 publications · 92 citations

    2

    h-index

  3. GJ
    Gwénaël Jouet

    Ifremer, France

    2 publications · 93 citations

    2

    h-index

  4. SJ
    Stéphan Jorry

    Ifremer, France

    2 publications · 93 citations

    2

    h-index

  5. PJ
    Peter J. Talling

    National Oceanography Centre, United Kingdom

    2 publications · 42 citations

    2

    h-index

1–5 of 86

Venues

  1. The Journal of Geology

    JG · 3 publications · 125 citations

    3

    h-index

  2. AAPG Bulletin

    2 publications · 549 citations

    2

    h-index

  3. Marine Geology

    2 publications · 71 citations

    2

    h-index

  4. Natural hazards and earth system sciences

    1 publications · 40 citations

    1

    h-index

  5. 1

    h-index

1–5