Abyssal Plain Sediments
**Abyssal Plain Sediments** is a deep-marine sedimentary facies consisting predominantly of fine-grained pelagic and hemipelagic particles, commonly interlayered with turbidites and other gravity-flow deposits, that accumulates on the flat, distal regions of ocean basins at abyssal depths and blankets the irregular topography of the underlying oceanic crust.
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2017–2026
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Serpentinization of abyssal peridotites at mid-ocean ridges
Catherine Mével · Comptes Rendus Géoscience · 2003 · 469 citations
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Woods Hole Oceanographic Institution, United States
6 publications · 417 citations
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National Oceanography Centre
Southampton, United Kingdom
19 h-index
56 publications
5.2K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
18 h-index
46 publications
3.1K citations

Centre National de la Recherche Scientifique
Paris, France
17 h-index
49 publications
4.5K citations
Woods Hole Oceanographic Institution
Falmouth, United States
15 h-index
25 publications
2K citations
Columbia University
New York, United States
14 h-index
29 publications
1.4K citations

Scripps Institution of Oceanography
La Jolla, United States
13 h-index
22 publications
1.1K citations
United States Geological Survey
Reston, United States
11 h-index
16 publications
764 citations
University of California San Diego
San Diego, United States
11 h-index
17 publications
887 citations
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44 publications · 2.4K citations
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20 publications · 670 citations
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17 publications · 1.2K citations
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16 publications · 1.3K citations
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JGR · 15 publications · 1.4K citations
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