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
Parents
148
Giorgio Rivalenti · Chemical Geology · 1993 · 631 citations
Bradley R. Hacker, P. B. Kelemen, M. D. Behn · Annual Review of Earth and Planetary Sciences · 2015 · 408 citations
1–5 of 148
439
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210
The University of Texas at Austin
Austin, United States
10 h-index
17 publications
1.6K citations
United States Geological Survey
Reston, United States
6 h-index
11 publications
3K citations
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
14 publications
1.2K citations

Chinese Academy of Sciences
Beijing, China
5 h-index
15 publications
786 citations

Australian National University
Canberra, Australia
5 h-index
11 publications
1.7K citations
University of Chicago
Chicago, United States
4 h-index
6 publications
518 citations
Planetary Science Institute
Tucson, United States
4 h-index
8 publications
1.4K citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
4 h-index
6 publications
428 citations
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JGR · 14 publications · 1.7K citations
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9 publications · 548 citations
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8 publications · 767 citations
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6 publications · 500 citations
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JGS · 5 publications · 538 citations
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