Contour Current Sedimentation
Contour Current Sedimentation is a geological sedimentation process in which sediments are transported and deposited along the seafloor by persistent, bottom-trapped oceanic currents that follow isobaths, distinguished from other sedimentation mechanisms by its reliance on deep-water contour-following currents driven by thermohaline circulation.
20
Publications
999
Citations
88
Authors
51
Institutions
Publications per year
2017–2026
5
Parents
20
1–5 of 20
88
2
h-index
National Institute of Oceanography and Applied Geophysics, Italy
2 publications · 143 citations
2
h-index
2
h-index
2
h-index
2
h-index
1–5 of 88
51
Université de Bordeaux
Bordeaux, France
3 h-index
12 publications
465 citations

China University of Petroleum, Beijing
Beijing, China
2 h-index
3 publications
171 citations

Zhejiang University
Hangzhou, China
2 h-index
5 publications
243 citations
Zhejiang Ocean University
Zhoushan, China
2 h-index
5 publications
243 citations
Environnements et Paléoenvironnements Océaniques et Continentaux
Pessac, France
2 h-index
9 publications
315 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
8 publications
328 citations
Institute of Oceanology
Qingdao, China
2 h-index
3 publications
103 citations
University of Cambridge
Cambridge, United Kingdom
2 h-index
4 publications
174 citations
1–8 of 51
3 publications · 155 citations
3
h-index
2 publications · 94 citations
2
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2 publications · 159 citations
2
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JSR · 2 publications · 107 citations
2
h-index
2 publications · 84 citations
2
h-index
1–5