Spinel Peridotite

Spinel Peridotite is a subclass of peridotite, a mantle rock composed predominantly of olivine and pyroxenes, distinguished by the presence of spinel as a primary refractory mineral phase stable at low to medium pressures in the Earth's upper mantle.

524

Publications

40.7K

Citations

1.1K

Authors

471

Institutions

Publications per year

2017–2026

79

Authors

1.1K

  1. SA
    Shoji Arai

    Kanazawa University, Japan

    32 publications · 2.4K citations

    20

    h-index

  2. DA
    Dmitri A. Ionov

    Université de Montpellier, France

    15 publications · 1.3K citations

    15

    h-index

  3. HD
    Hilary Downes

    Birkbeck, University of London, United Kingdom

    10 publications · 726 citations

    10

    h-index

  4. JL
    Jean-Pierre Lorand

    Centre National de la Recherche Scientifique, France

    10 publications · 766 citations

    10

    h-index

  5. CJ
    Carlos J. Garrido

    Instituto Andaluz de Ciencias de la Tierra, Spain

    8 publications · 675 citations

    8

    h-index

1–5 of 1.1K

Venues

  1. Journal of Petrology

    76 publications · 7K citations

    49

    h-index

  2. Contributions to Mineralogy and Petrology

    43 publications · 6.2K citations

    31

    h-index

  3. Earth and Planetary Science Letters

    27 publications · 3.5K citations

    24

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 24 publications · 4.1K citations

    22

    h-index

  5. Geochimica et Cosmochimica Acta

    19 publications · 1.5K citations

    19

    h-index

1–5