Core-mantle Equilibrium

Core-Mantle Equilibrium is a geochemical model that describes the state of chemical and isotopic partitioning between Earth's metallic core and silicate mantle achieved through high-pressure, high-temperature equilibration during planetary differentiation.

444

Publications

35.9K

Citations

940

Authors

353

Institutions

Publications per year

2017–2026

75

Authors

940

  1. RJ
    Raymond Jeanloz

    University of California, Berkeley, United States

    14 publications · 2.4K citations

    14

    h-index

  2. EO
    Eiji Ohtani

    Tohoku University, Japan

    10 publications · 361 citations

    10

    h-index

  3. KD
    Konstantin D. Litasov

    V.S. Sobolev Institute of Geology and Mineralogy, Russia

    9 publications · 316 citations

    9

    h-index

  4. DC
    D. C. Rubie

    University of Bayreuth, Germany

    9 publications · 1.3K citations

    9

    h-index

  5. DW
    David Walker

    Lamont-Doherty Earth Observatory, United States

    9 publications · 646 citations

    9

    h-index

1–5 of 940

Venues

  1. Earth and Planetary Science Letters

    71 publications · 6.1K citations

    41

    h-index

  2. Physics of The Earth and Planetary Interiors

    57 publications · 3.7K citations

    34

    h-index

  3. Geophysical Research Letters

    41 publications · 2.4K citations

    31

    h-index

  4. Nature

    27 publications · 4.3K citations

    25

    h-index

  5. Geochimica et Cosmochimica Acta

    25 publications · 2K citations

    22

    h-index

1–5