Gabbroic Plutons

Gabbroic Plutons is a geological construct referring to large, intrusive igneous bodies formed by the slow crystallization of magnesium- and iron-rich magma beneath mid-ocean ridges, distinguishing it from extrusive basaltic formations and smaller-scale mafic intrusions in oceanic crustal accretion models.

853

Publications

51.7K

Citations

2.4K

Authors

735

Institutions

Publications per year

2017–2026

113

Authors

2.4K

  1. SM
    Sandra M. Barr

    Acadia University, Canada

    14 publications · 319 citations

    12

    h-index

  2. GP
    Georgia Pe‐Piper

    Saint Mary's University, Canada

    10 publications · 282 citations

    10

    h-index

  3. FC
    Fernando Corfú

    University of Oslo, Norway

    9 publications · 652 citations

    9

    h-index

  4. RT
    Riccardo Tribuzio

    University of Pavia, Italy

    8 publications · 285 citations

    8

    h-index

  5. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    8 publications · 290 citations

    8

    h-index

1–5 of 2.4K

Venues

  1. Lithos

    71 publications · 5.8K citations

    34

    h-index

  2. Contributions to Mineralogy and Petrology

    46 publications · 3.7K citations

    33

    h-index

  3. Precambrian Research

    45 publications · 2.7K citations

    31

    h-index

  4. Journal of Petrology

    41 publications · 2.8K citations

    28

    h-index

  5. Earth and Planetary Science Letters

    35 publications · 3.7K citations

    28

    h-index

1–5