Bottom Current Processes
Bottom Current Processes is a sediment transport mechanism belonging to the class of deep-marine and lacustrine depositional processes, distinguished by the persistent movement of density-driven, near-bottom water flows that selectively erode, transport, and deposit fine-grained sediments along continental slopes and basin floors.
161
Publications
6.5K
Citations
499
Authors
222
Institutions
Publications per year
2017–2026
29
161
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 161
499
Royal Holloway University of London, United Kingdom
10 publications · 597 citations
10
h-index
6
h-index
6
h-index
National Institute of Oceanography and Applied Geophysics, Italy
5 publications · 209 citations
5
h-index
5
h-index
1–5 of 499
222

Royal Holloway University of London
Egham, United Kingdom
10 h-index
15 publications
432 citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
9 h-index
18 publications
446 citations
National Institute of Oceanography and Applied Geophysics
Trieste, Italy
9 h-index
38 publications
1.7K citations

National Oceanography Centre
Southampton, United Kingdom
7 h-index
9 publications
810 citations

British Geological Survey
Nottingham, United Kingdom
7 h-index
12 publications
617 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
7 h-index
8 publications
294 citations
Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche
Venice, Italy
6 h-index
18 publications
748 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
10 publications
301 citations
1–8 of 222
34 publications · 1.3K citations
22
h-index
JGR · 8 publications · 355 citations
8
h-index
6 publications · 263 citations
6
h-index
5 publications · 179 citations
5
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5 publications · 265 citations
5
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1–5