Gravity-driven Sedimentation
Gravity-Driven Sedimentation is a geological process in which slope sediments are transported and deposited under the influence of gravitational forces, distinguished from other sedimentation mechanisms by its primary reliance on gravity-induced downslope movement such as landslides, debris flows, and turbidity currents.
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Revision of kynch sedimentation theory
Frank M. Tiller · AIChE Journal · 1981 · 121 citations
Lincoln F. Pratson, Edward P. Laine · Marine Geology · 1989 · 99 citations
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Chinese Academy of Sciences
Beijing, China
3 h-index
3 publications
82 citations
Research Institute of Petroleum Exploration and Development
Beijing, China
3 h-index
15 publications
314 citations
Sinopec (China)
Beijing, China
2 h-index
4 publications
92 citations

Xi'an Shiyou University
Xi'an, China
2 h-index
3 publications
47 citations

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

Cornell University
Ithaca, United States
2 h-index
6 publications
225 citations
Universität Hamburg
Hamburg, Germany
2 h-index
4 publications
50 citations
Institute for Biodiversity
Regensburg, Germany
2 h-index
2 publications
40 citations
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6 publications · 201 citations
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