Turbidity Current Deposition is a geological sedimentation process in which sediment-laden, gravity-driven flows of water descend submarine slopes and deposit graded beds of sand, silt, and clay in deep-marine environments, distinguished from other depositional processes by its reliance on density differences generated by suspended sediment concentration.
358
Publications
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Citations
775
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368
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Publications per year
2017–2026
54
Publications
358
Turbidity Currents as a Cause of Graded Bedding
Ph. H. Kuenen, C. I. Migliorini · The Journal of Geology · 1950 · 550 citations
Turbidity Currents and Their Deposits
Eckart Meiburg, Ben Kneller · Annual Review of Fluid Mechanics · 2010 · 509 citations
1–5 of 358
Authors
775
- PJ
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11
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10
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1–5 of 775
Institutions
368
Geological Survey of Canada
Ottawa, Canada
18 h-index
30 publications
2.5K citations
University of Leeds
Leeds, United Kingdom
18 h-index
36 publications
2.8K citations
Shell (United States)
Houston, United States
15 h-index
36 publications
2.5K citations
University of Minnesota
Minneapolis, United States
12 h-index
19 publications
1.3K citations
Utrecht University
Utrecht, The Netherlands
12 h-index
23 publications
1.3K citations
National Oceanography Centre
Southampton, United Kingdom
12 h-index
43 publications
5K citations
Bedford Institute of Oceanography
Dartmouth, Canada
12 h-index
13 publications
1.3K citations
University of South Carolina
Columbia, United States
10 h-index
19 publications
1.4K citations
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Venues
- Journal of Sedimentary Research
JSR · 53 publications · 4.3K citations
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- Sedimentology
55 publications · 3.7K citations
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- AAPG Bulletin
18 publications · 1K citations
16
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- Sedimentary Geology
12 publications · 647 citations
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- The Journal of Geology
JG · 12 publications · 1.3K citations
12
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