Accretionary Orogens

Accretionary Orogens is a tectonic model of mountain building characterized by the gradual growth of continental crust through the accretion of oceanic and continental terranes at convergent plate margins, distinguishing it from collisional orogens that form primarily by continent-continent convergence.

1.1K

Publications

108.4K

Citations

2.8K

Authors

731

Institutions

Publications per year

2017–2026

276

Authors

2.8K

  1. WX
    Wenjiao Xiao

    Chinese Academy of Sciences, China

    46 publications · 10.4K citations

    32

    h-index

  2. BF
    Brian F. Windley

    University of Leicester, United Kingdom

    38 publications · 13.5K citations

    29

    h-index

  3. MS
    Min Sun

    University of Hong Kong, Hong Kong SAR China

    35 publications · 9.5K citations

    29

    h-index

  4. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    23 publications · 5.3K citations

    21

    h-index

  5. PA
    Peter A. Cawood

    Monash University, Australia

    21 publications · 5.9K citations

    20

    h-index

1–5 of 2.8K

Venues

  1. Precambrian Research

    140 publications · 12.6K citations

    60

    h-index

  2. Gondwana Research

    76 publications · 10.7K citations

    45

    h-index

  3. Tectonophysics

    70 publications · 8.7K citations

    42

    h-index

  4. Geology

    39 publications · 4.4K citations

    31

    h-index

  5. Geological Society London Special Publications

    41 publications · 4.5K citations

    29

    h-index

1–5