Crustal Accretion

Crustal Accretion is a geophysical process in which new oceanic crust is formed through the localized intrusion and extrusion of magma at mid-ocean ridges, distinguishing it from other crustal formation mechanisms by its continuous, seafloor-spreading-driven addition of igneous material to the lithosphere.

600

Publications

49.2K

Citations

1.9K

Authors

593

Institutions

Publications per year

2017–2026

114

Authors

1.9K

  1. BF
    Brian F. Windley

    University of Leicester, United Kingdom

    9 publications · 1.1K citations

    9

    h-index

  2. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    9 publications · 1.1K citations

    9

    h-index

  3. BI
    Benoı̂t Ildefonse

    Université de Montpellier, France

    8 publications · 606 citations

    8

    h-index

  4. JP
    J. P. Canales

    Woods Hole Oceanographic Institution, United States

    7 publications · 460 citations

    7

    h-index

  5. MJ
    Martin J. Whitehouse

    Swedish Museum of Natural History, Sweden

    7 publications · 550 citations

    7

    h-index

1–5 of 1.9K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 49 publications · 4.3K citations

    35

    h-index

  2. Precambrian Research

    46 publications · 4.8K citations

    32

    h-index

  3. Geology

    40 publications · 3.4K citations

    30

    h-index

  4. Earth and Planetary Science Letters

    30 publications · 2.8K citations

    28

    h-index

  5. Geochemistry Geophysics Geosystems

    24 publications · 3.5K citations

    21

    h-index

1–5