High-density Turbidity Currents
High-Density Turbidity Currents is a type of sediment gravity flow characterized by high sediment concentration and turbulent fluid support, distinguished from low-density counterparts by its ability to generate grain-to-grain interactions and sustained turbulent suspension, resulting in massive to normally graded bedding with distinctive erosional and depositional structures in deep-marine environments.
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2017–2026
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Turbidity Currents as a Cause of Graded Bedding
Ph. H. Kuenen, C. I. Migliorini · The Journal of Geology · 1950 · 550 citations
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University of Leeds
Leeds, United Kingdom
5 h-index
6 publications
923 citations
ExxonMobil (United States)
Irving, United States
3 h-index
3 publications
619 citations

University of Bristol
Bristol, United Kingdom
3 h-index
7 publications
248 citations

Delft University of Technology
Delft, The Netherlands
3 h-index
6 publications
189 citations
Geological Survey of Canada
Ottawa, Canada
3 h-index
5 publications
227 citations
Instytut Nauk Geologicznych
Warsaw, Poland
3 h-index
5 publications
198 citations

Heriot-Watt University
Edinburgh, United Kingdom
2 h-index
5 publications
188 citations
University of Illinois Urbana-Champaign
Urbana, United States
2 h-index
2 publications
52 citations
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JSR · 14 publications · 3.5K citations
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8 publications · 1.2K citations
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7 publications · 488 citations
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5 publications · 197 citations
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4 publications · 195 citations
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