Delta Sedimentation
Delta Sedimentation is a geomorphological process denoting the depositional accumulation of clastic sediments at a river mouth, distinguished by the construction of subaerial and subaqueous deltaic landforms through the interaction of fluvial discharge, sediment load, and receiving basin dynamics.
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Publications
27.7K
Citations
1.3K
Authors
480
Institutions
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2017–2026
115
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480

East China Normal University
Shanghai, China
23 h-index
103 publications
6.4K citations

Ocean University of China
Qingdao, China
23 h-index
102 publications
6.6K citations
Louisiana State University
Baton Rouge, United States
20 h-index
56 publications
3.4K citations
Geological Survey of Japan
Tsukuba, Japan
19 h-index
31 publications
3.5K citations
Qingdao Institute of Marine Geology
Qingdao, China
17 h-index
54 publications
3.8K citations

Chinese Academy of Sciences
Beijing, China
16 h-index
63 publications
2.4K citations
Qingdao National Laboratory for Marine Science and Technology
Qingdao, China
16 h-index
53 publications
2.5K citations
Nanjing University
Nanjing, China
12 h-index
21 publications
1.5K citations
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36 publications · 3.1K citations
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19 publications · 2.2K citations
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JCR · 16 publications · 760 citations
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16 publications · 1.1K citations
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12 publications · 929 citations
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