Isostatic Equilibrium

Isostatic Equilibrium is a geophysical state in which the Earth's lithosphere achieves static balance over the asthenosphere due to buoyant forces counteracting surface load changes, such that vertical crustal motions cease in response to glacial or oceanic mass redistribution.

180

Publications

11.8K

Citations

376

Authors

198

Institutions

Publications per year

2017–2026

17

Variants

Isostasy

Authors

376

  1. PM
    Péter Molnár

    Massachusetts Institute of Technology, United States

    8 publications · 1.2K citations

    8

    h-index

  2. RJ
    R. J. Phillips

    Southwest Research Institute, United States

    3 publications · 137 citations

    3

    h-index

  3. CL
    Cheng‐Horng Lin

    Institute of Earth Sciences, Academia Sinica, Taiwan

    3 publications · 47 citations

    3

    h-index

  4. HL
    H. Lyon‐Caen

    Centre National de la Recherche Scientifique, France

    3 publications · 603 citations

    3

    h-index

  5. JE
    J. Ebbing

    Geological Survey of Norway, Norway

    3 publications · 125 citations

    3

    h-index

1–5 of 376

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 33 publications · 2.3K citations

    24

    h-index

  2. Geophysical Journal International

    GJI · 23 publications · 1K citations

    18

    h-index

  3. Geophysical Research Letters

    12 publications · 922 citations

    12

    h-index

  4. Geological Society London Special Publications

    6 publications · 158 citations

    6

    h-index

  5. Physical Review Letters

    PRL · 6 publications · 387 citations

    6

    h-index

1–5