Gabbroic Accretion

Gabbroic Accretion is a geological process in which new oceanic crust is formed at mid-ocean ridges through the sequential crystallization and emplacement of gabbroic rocks from differentiated magma chambers beneath the seafloor.

215

Publications

13.8K

Citations

711

Authors

320

Institutions

Publications per year

2017–2026

31

Authors

711

  1. HJ
    H. J. Dick

    Woods Hole Oceanographic Institution, United States

    9 publications · 768 citations

    9

    h-index

  2. RT
    Riccardo Tribuzio

    University of Pavia, Italy

    8 publications · 305 citations

    8

    h-index

  3. MJ
    M. J. Cheadle

    University of Wyoming, United States

    7 publications · 609 citations

    7

    h-index

  4. BI
    Benoı̂t Ildefonse

    Université de Montpellier, France

    7 publications · 385 citations

    7

    h-index

  5. TN
    Toshio Nozaka

    Okayama University, Japan

    6 publications · 379 citations

    6

    h-index

1–5 of 711

Venues

  1. Lithos

    17 publications · 697 citations

    14

    h-index

  2. Contributions to Mineralogy and Petrology

    12 publications · 751 citations

    12

    h-index

  3. Earth and Planetary Science Letters

    14 publications · 930 citations

    12

    h-index

  4. Journal of Petrology

    10 publications · 523 citations

    10

    h-index

  5. Precambrian Research

    8 publications · 555 citations

    8

    h-index

1–5