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

Authors

883

  1. ZA
    Zhisheng An

    Institute of Earth Environment, China

    14 publications · 1.5K citations

    13

    h-index

  2. SY
    Shiling Yang

    Institute of Geology and Geophysics, China

    12 publications · 1.7K citations

    12

    h-index

  3. ZL
    Z. L. Ding

    Chinese Academy of Sciences, China

    11 publications · 1.7K citations

    11

    h-index

  4. JN
    Junsheng Nie

    Lanzhou University, China

    10 publications · 424 citations

    10

    h-index

  5. YS
    Yougui Song

    Institute of Earth Environment, China

    10 publications · 767 citations

    10

    h-index

1–5 of 883

Venues

  1. Palaeogeography Palaeoclimatology Palaeoecology

    21 publications · 1.4K citations

    18

    h-index

  2. Journal of Sedimentary Research

    JSR · 12 publications · 615 citations

    12

    h-index

  3. Sedimentary Geology

    13 publications · 414 citations

    12

    h-index

  4. Geophysical Research Letters

    11 publications · 860 citations

    11

    h-index

  5. CATENA

    8 publications · 221 citations

    8

    h-index

1–5