Subduction-collision Transition

Subduction-Collision Transition is a geodynamic process denoting the shift from oceanic subduction to continental collision within convergent plate margins, characterized by the cessation of slab pull and the onset of crustal thickening due to buoyant continental lithosphere entering the subduction zone.

279

Publications

24.6K

Citations

1K

Authors

438

Institutions

Publications per year

2017–2026

73

Authors

1K

  1. TG
    Taras Gerya

    ETH Zurich, Switzerland

    8 publications · 686 citations

    8

    h-index

  2. CL
    Char‐Shine Liu

    National Taiwan University, Taiwan

    7 publications · 521 citations

    7

    h-index

  3. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    6 publications · 249 citations

    6

    h-index

  4. CB
    Christopher Beaumont

    Dalhousie University, Canada

    5 publications · 848 citations

    5

    h-index

  5. LZ
    Lifei Zhang

    Peking University, China

    5 publications · 705 citations

    5

    h-index

1–5 of 1K

Venues

  1. Tectonophysics

    31 publications · 2.6K citations

    23

    h-index

  2. Earth and Planetary Science Letters

    17 publications · 2.7K citations

    16

    h-index

  3. Lithos

    16 publications · 1.5K citations

    16

    h-index

  4. Gondwana Research

    15 publications · 637 citations

    14

    h-index

  5. Tectonics

    12 publications · 798 citations

    12

    h-index

1–5