Lithospheric Cooling

Lithospheric Cooling is a geophysical process in which the oceanic lithosphere gradually loses heat to the overlying hydrosphere and atmosphere as it moves away from a mid-ocean ridge, resulting in progressive thermal contraction, thickening, and increased density with age.

161

Publications

11.6K

Citations

359

Authors

195

Institutions

Publications per year

2017–2026

12

Authors

359

  1. MD
    Marie‐Pierre Doin

    Centre National de la Recherche Scientifique, France

    6 publications · 368 citations

    6

    h-index

  2. SS
    Seth Stein

    Northwestern University, United States

    6 publications · 818 citations

    6

    h-index

  3. AC
    Anny Cazenave

    Laboratoire d’Études en Géophysique et Océanographie Spatiales, France

    6 publications · 209 citations

    6

    h-index

  4. CA
    Carol A. Stein

    University of Illinois Chicago, United States

    5 publications · 781 citations

    5

    h-index

  5. EM
    E. M. Parmentier

    Brown University, United States

    5 publications · 368 citations

    5

    h-index

1–5 of 359

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 27 publications · 2.6K citations

    22

    h-index

  2. Earth and Planetary Science Letters

    21 publications · 1.7K citations

    21

    h-index

  3. Tectonophysics

    15 publications · 1.6K citations

    13

    h-index

  4. Geophysical Research Letters

    12 publications · 404 citations

    12

    h-index

  5. Nature

    11 publications · 1.5K citations

    10

    h-index

1–5