Bottom Current Sedimentation
Bottom Current Sedimentation is a sedimentary process within deep-sea environments characterized by the selective erosion, transport, and deposition of sediments by persistent near-bottom density-driven currents, distinguishing it from other deep-sea sedimentation mechanisms through its association with contour-following flow dynamics and formation of contourite deposits.
91
Publications
4K
Citations
325
Authors
166
Institutions
Publications per year
2017–2026
17
Variants
Contourite Sedimentation
91
Deep water bottom current deposition in the northern South China Sea
Lei Shao, Xuejie Li, Jianhua Geng et al. · Science in China Series D Earth Sciences · 2007 · 145 citations
1–5 of 91
325
Royal Holloway University of London, United Kingdom
5 publications · 165 citations
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4
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4
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3
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3
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1–5 of 325
166

Royal Holloway University of London
Egham, United Kingdom
8 h-index
10 publications
386 citations
University of Bremen
Bremen, Germany
6 h-index
16 publications
794 citations

Ghent University
Ghent, Belgium
6 h-index
14 publications
502 citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
6 h-index
9 publications
191 citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
12 publications
676 citations

Instituto Geológico y Minero de España
Madrid, Spain
4 h-index
6 publications
202 citations

Universidade de Vigo
Vigo, Spain
4 h-index
8 publications
443 citations
National Institute of Oceanography and Applied Geophysics
Trieste, Italy
4 h-index
16 publications
762 citations
1–8 of 166
24 publications · 985 citations
18
h-index
7 publications · 491 citations
7
h-index
4 publications · 124 citations
4
h-index
4 publications · 99 citations
4
h-index
3 publications · 118 citations
3
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1–5