Accretionary Orogenesis

Accretionary Orogenesis is a geological process, within the broader category of orogenic development, that specifically involves the growth of continental margins through the progressive addition of accreted terranes at convergent plate boundaries.

1.1K

Publications

105.6K

Citations

3K

Authors

769

Institutions

Publications per year

2017–2026

295

Authors

3K

  1. WX
    Wenjiao Xiao

    Chinese Academy of Sciences, China

    52 publications · 9.1K citations

    36

    h-index

  2. MS
    Min Sun

    University of Hong Kong, Hong Kong SAR China

    43 publications · 10.3K citations

    35

    h-index

  3. BF
    Brian F. Windley

    University of Leicester, United Kingdom

    38 publications · 11.5K citations

    31

    h-index

  4. PA
    Peter A. Cawood

    Monash University, Australia

    29 publications · 7.3K citations

    25

    h-index

  5. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    24 publications · 3.5K citations

    22

    h-index

1–5 of 3K

Venues

  1. Precambrian Research

    124 publications · 12.3K citations

    60

    h-index

  2. Gondwana Research

    94 publications · 10.4K citations

    50

    h-index

  3. Tectonophysics

    59 publications · 5.5K citations

    39

    h-index

  4. Lithos

    66 publications · 4.2K citations

    37

    h-index

  5. Journal of Asian Earth Sciences

    51 publications · 7.2K citations

    33

    h-index

1–5