Mantle Upwelling

Mantle Upwelling is a geophysical process in which buoyant, thermally activated mantle material rises from deeper regions of the Earth's interior toward the surface, driven by thermal convection and decompression melting, particularly beneath divergent plate boundaries such as mid-ocean ridges and continental rift zones.

327

Publications

24K

Citations

914

Authors

379

Institutions

Publications per year

2017–2026

74

Authors

914

  1. EM
    E. M. Parmentier

    Brown University, United States

    7 publications · 542 citations

    7

    h-index

  2. DK
    Derek Keir

    University of Southampton, United Kingdom

    5 publications · 272 citations

    5

    h-index

  3. SS
    Stephen S. Gao

    Missouri University of Science and Technology, United States

    5 publications · 118 citations

    5

    h-index

  4. DZ
    Dapeng Zhao

    Tohoku University, Japan

    5 publications · 207 citations

    5

    h-index

  5. DZ
    Dapeng Zhao

    Tohoku University, Japan

    5 publications · 302 citations

    5

    h-index

1–5 of 914

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 37 publications · 4.2K citations

    34

    h-index

  2. Geophysical Research Letters

    35 publications · 1.7K citations

    24

    h-index

  3. Earth and Planetary Science Letters

    26 publications · 1.9K citations

    23

    h-index

  4. Geochemistry Geophysics Geosystems

    20 publications · 1.2K citations

    17

    h-index

  5. Geophysical Journal International

    GJI · 20 publications · 1.2K citations

    17

    h-index

1–5