Orogenic Belt Reconstruction

Orogenic Belt Reconstruction is a tectonic reconstruction method that specifically restores the structural and spatial evolution of mountain belts formed by continental collision, subduction, or crustal shortening, distinguishing itself from broader plate-scale reconstructions by focusing on the geometry, kinematics, and timing of orogen-parallel and orogen-perpendicular deformation processes.

1.6K

Publications

122.4K

Citations

4.3K

Authors

824

Institutions

Publications per year

2017–2026

511

Authors

4.3K

  1. WX
    Wenjiao Xiao

    Chinese Academy of Sciences, China

    54 publications · 6.3K citations

    35

    h-index

  2. MS
    Min Sun

    University of Hong Kong, Hong Kong SAR China

    50 publications · 7.2K citations

    34

    h-index

  3. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    41 publications · 5.1K citations

    32

    h-index

  4. GZ
    Guochun Zhao

    University of Hong Kong, Hong Kong SAR China

    37 publications · 6.4K citations

    28

    h-index

  5. SA
    Simon A. Wilde

    Curtin University, Australia

    23 publications · 5.5K citations

    23

    h-index

1–5 of 4.3K

Venues

  1. Gondwana Research

    123 publications · 15.5K citations

    59

    h-index

  2. Precambrian Research

    121 publications · 10.1K citations

    57

    h-index

  3. Journal of Asian Earth Sciences

    151 publications · 11.1K citations

    56

    h-index

  4. Lithos

    124 publications · 8.2K citations

    52

    h-index

  5. Tectonophysics

    93 publications · 10.9K citations

    45

    h-index

1–5