Sediment Load Effects

Sediment Load Effects is a geophysical phenomenon within the study of Glacial Isostatic Adjustment that refers to the deformation of the Earth's crust resulting from the accumulation and redistribution of sedimentary material, distinguished from other isostatic forcing mechanisms by its dependence on erosional-depositional processes rather than ice-mass or ocean-load changes.

168

Publications

9.5K

Citations

557

Authors

254

Institutions

Publications per year

2017–2026

45

Authors

557

  1. WS
    Wenyi Sun

    Institute of Soil and Water Conservation, China

    5 publications · 272 citations

    5

    h-index

  2. XM
    Xingmin Mu

    Institute of Soil and Water Conservation, China

    5 publications · 272 citations

    5

    h-index

  3. PG
    Peng Gao

    Institute of Soil and Water Conservation, China

    5 publications · 272 citations

    5

    h-index

  4. GZ
    Guangju Zhao

    Institute of Soil and Water Conservation, China

    4 publications · 181 citations

    4

    h-index

  5. XZ
    XC Zhang

    Grazinglands Research Laboratory, United States

    3 publications · 176 citations

    3

    h-index

1–5 of 557

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 8 publications · 1.1K citations

    8

    h-index

  2. Journal of Hydrology

    5 publications · 166 citations

    5

    h-index

  3. Scientific Reports

    4 publications · 276 citations

    4

    h-index

  4. CATENA

    4 publications · 187 citations

    4

    h-index

  5. Geophysical Research Letters

    3 publications · 131 citations

    3

    h-index

1–5