Slope Depositional Environments
Slope Depositional Environments is a marine sedimentary environment characterized by its occurrence on the inclined transition zone between the continental shelf and the deep ocean floor, distinguished from other depositional settings by its moderate to steep gradients, gravitational sediment transport processes, and accumulation of mass-transport deposits and turbidites.
149
Publications
5.8K
Citations
457
Authors
203
Institutions
Publications per year
2017–2026
16
Variants
Continental Slope Depositional Environments
Parents
149
New U–Pb zircon ages of the Ediacaran–Cambrian boundary strata in South China
Daizhao Chen, Xiqiang Zhou, Yong Fu et al. · Terra Nova · 2014 · 177 citations
Kerrie L. Bann, Christopher R. Fielding, James A. MacEachern et al. · Geological Society London Special Publications · 2004 · 142 citations
1–5 of 149
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203
The University of Texas at Austin
Austin, United States
5 h-index
7 publications
187 citations
United States Geological Survey
Reston, United States
5 h-index
5 publications
259 citations
Queen's University
Kingston, Canada
4 h-index
10 publications
958 citations

Chinese Academy of Sciences
Beijing, China
4 h-index
7 publications
678 citations
Research Institute of Petroleum Exploration and Development
Beijing, China
4 h-index
13 publications
467 citations
National Institute of Oceanography
Panjim, India
3 h-index
5 publications
65 citations

University of Alberta
Edmonton, Canada
3 h-index
4 publications
182 citations
Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
6 publications
322 citations
1–8 of 203
14 publications · 406 citations
13
h-index
9 publications · 639 citations
9
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JSR · 8 publications · 352 citations
8
h-index
8 publications · 448 citations
8
h-index
6 publications · 266 citations
6
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1–5