Red Clay Sediments
Red Clay Sediment is a type of pelagic sediment predominantly composed of fine-grained terrigenous clay minerals and authigenic particles, distinguished by its reddish color due to iron oxide coatings and its occurrence in the deepest, most remote regions of the ocean floor where other sediment sources are minimal.
320
Publications
14.9K
Citations
883
Authors
342
Institutions
Publications per year
2017–2026
49
Variants
Abyssal Red ClayPelagic Red Clay
Parents
320
Z. L. Ding, Shangfa Xiong, Jimin Sun et al. · Palaeogeography Palaeoclimatology Palaeoecology · 1999 · 355 citations
1–5 of 320
883
13
h-index
12
h-index
11
h-index
10
h-index
10
h-index
1–5 of 883
342

Chinese Academy of Sciences
Beijing, China
36 h-index
219 publications
20.6K citations
Institute of Earth Environment
Xi'an, China
27 h-index
89 publications
10.3K citations
Institute of Geology and Geophysics
Beijing, China
22 h-index
71 publications
5.4K citations
Lanzhou University
Lanzhou, China
12 h-index
30 publications
1.4K citations
Northwest University
Xi'an, China
10 h-index
32 publications
1.4K citations
Institute of Tibetan Plateau Research
Beijing, China
9 h-index
19 publications
702 citations
Institute of Soil Science
Nanjing, China
9 h-index
17 publications
591 citations

China Geological Survey
Beijing, China
8 h-index
25 publications
523 citations
1–8 of 342
21 publications · 1.4K citations
18
h-index
JSR · 12 publications · 615 citations
12
h-index
13 publications · 414 citations
12
h-index
11 publications · 860 citations
11
h-index
8 publications · 221 citations
8
h-index
1–5