Sediment Subduction

Sediment Subduction is the geophysical process in which terrigenous and pelagic sediments are transported into the Earth's mantle along a subducting oceanic plate at a convergent plate boundary, distinguished from other forms of subduction by the specific inclusion and deep recycling of surface-derived sedimentary material.

148

Publications

14.1K

Citations

439

Authors

210

Institutions

Publications per year

2017–2026

27

Authors

439

  1. GF
    Gregory F. Moore

    University of Hawaii System, United States

    6 publications · 281 citations

    6

    h-index

  2. RV
    Roland von Huene

    United States Geological Survey, United States

    5 publications · 1.6K citations

    5

    h-index

  3. TH
    Thomas H. Shipley

    The University of Texas at Austin, United States

    4 publications · 180 citations

    4

    h-index

  4. DW
    David W. Scholl

    United States Geological Survey, United States

    3 publications · 1.5K citations

    3

    h-index

  5. PJ
    Peter J. Wyllie

    University of Chicago, United States

    3 publications · 420 citations

    3

    h-index

1–5 of 439

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 14 publications · 1.7K citations

    14

    h-index

  2. Earth and Planetary Science Letters

    9 publications · 548 citations

    9

    h-index

  3. Geology

    8 publications · 767 citations

    8

    h-index

  4. Gondwana Research

    6 publications · 500 citations

    6

    h-index

  5. Journal of the Geological Society

    JGS · 5 publications · 538 citations

    5

    h-index

1–5