Syn-rift Sedimentation
Syn-Rift Sedimentation is a geological process category of sedimentation that occurs contemporaneously with active crustal extension and faulting during continental rifting, distinguished by its temporal and spatial association with tectonic deformation in rift basins.
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2017–2026
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Ingrid Ukstins Peate, Paul R. Renne, E. Wolfenden et al. · Earth and Planetary Science Letters · 2002 · 250 citations
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Centre National de la Recherche Scientifique
Paris, France
15 h-index
35 publications
1.7K citations
University of Bergen
Bergen, Norway
11 h-index
19 publications
913 citations
China University of Geosciences
Wuhan, China
11 h-index
31 publications
1.3K citations

China University of Geosciences (Beijing)
Beijing, China
10 h-index
27 publications
722 citations
Geological Survey of Denmark and Greenland
Copenhagen, Denmark
9 h-index
32 publications
1.2K citations

Royal Holloway University of London
Egham, United Kingdom
9 h-index
20 publications
1.7K citations

China National Offshore Oil Corporation (China)
Beijing, China
8 h-index
13 publications
579 citations

China University of Petroleum, Beijing
Beijing, China
8 h-index
29 publications
515 citations
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32 publications · 1.1K citations
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