Margin Subsidence

Margin Subsidence is a geological process denoting the gradual downward movement of the Earth's crust along continental margins, distinguished by lithospheric cooling, sediment loading, and tectonic forces that collectively drive vertical crustal deformation in passive or active margin settings.

56

Publications

4.8K

Citations

178

Authors

99

Institutions

Publications per year

2017–2026

9

Authors

178

  1. DW
    David W. Scholl

    United States Geological Survey, United States

    2 publications · 267 citations

    2

    h-index

  2. AH
    Alastair H.F. Robertson

    University of Edinburgh, United Kingdom

    2 publications · 288 citations

    2

    h-index

  3. SC
    Sierd Cloetingh

    Vrije Universiteit Amsterdam, Netherlands

    2 publications · 265 citations

    2

    h-index

  4. OE
    Olav Eldholm

    University of Oslo, Norway

    2 publications · 189 citations

    2

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  5. DL
    Daniel Lizarralde

    Woods Hole Oceanographic Institution, United States

    2 publications · 212 citations

    2

    h-index

1–5 of 178

Venues

  1. Tectonophysics

    7 publications · 419 citations

    7

    h-index

  2. Earth and Planetary Science Letters

    5 publications · 951 citations

    5

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 5 publications · 505 citations

    5

    h-index

  4. Geological Society London Special Publications

    4 publications · 229 citations

    4

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  5. Journal of the Geological Society

    JGS · 3 publications · 230 citations

    3

    h-index

1–5