Tectonic Plate Divergence

Tectonic Plate Divergence is a geological process in which two lithospheric plates move away from each other at a divergent boundary, resulting in the upwelling of magma from the mantle and the formation of new oceanic crust at mid-ocean ridges.

143

Publications

19.8K

Citations

384

Authors

226

Institutions

Publications per year

2017–2026

24

Variants

Plate Divergence

Authors

384

  1. GM
    Gérard M. Stampfli

    University of Lausanne, Switzerland

    3 publications · 2.8K citations

    3

    h-index

  2. GE
    Graeme Eagles

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    3 publications · 373 citations

    3

    h-index

  3. MC
    Mathilde Cannat

    Institut de physique du globe de Paris, France

    3 publications · 80 citations

    3

    h-index

  4. DS
    D. Sarah Stamps

    Virginia Tech, United States

    2 publications · 143 citations

    2

    h-index

  5. GB
    Gilles Borel

    University of Lausanne, Switzerland

    2 publications · 2.6K citations

    2

    h-index

1–5 of 384

Venues

  1. Tectonophysics

    17 publications · 5.9K citations

    15

    h-index

  2. Geological Society London Special Publications

    8 publications · 656 citations

    8

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 7 publications · 512 citations

    7

    h-index

  4. Geology

    7 publications · 624 citations

    7

    h-index

  5. Earth and Planetary Science Letters

    6 publications · 2.9K citations

    6

    h-index

1–5