Bottom Current Deposits
Bottom Current Deposits is a type of deep-marine sedimentary deposit characterized by its formation from the reworking and accumulation of sediments transported and winnowed by persistent bottom-intensified ocean currents, distinguishing it from deposits primarily formed by turbidity flows or pelagic settling.
99
Publications
4.1K
Citations
291
Authors
149
Institutions
Publications per year
2017–2026
14
Parents
99
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 99
291
Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche, Italy
5 publications · 287 citations
5
h-index
5
h-index
4
h-index
Royal Holloway University of London, United Kingdom
4 publications · 151 citations
4
h-index
3
h-index
1–5 of 291
149

Royal Holloway University of London
Egham, United Kingdom
6 h-index
10 publications
483 citations
National Institute of Oceanography and Applied Geophysics
Trieste, Italy
5 h-index
17 publications
776 citations
Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche
Venice, Italy
5 h-index
11 publications
443 citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
5 h-index
9 publications
196 citations

Ghent University
Ghent, Belgium
4 h-index
10 publications
363 citations
Instituto Andaluz de Ciencias de la Tierra
Granada, Spain
4 h-index
4 publications
204 citations
Université de Bordeaux
Bordeaux, France
4 h-index
11 publications
524 citations
The University of Texas at Arlington
Arlington, United States
4 h-index
4 publications
240 citations
1–8 of 149
19 publications · 566 citations
15
h-index
7 publications · 273 citations
7
h-index
5 publications · 209 citations
5
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4 publications · 254 citations
4
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4 publications · 351 citations
4
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1–5