Orogenic Belts

Orogenic Belts is a geological structure characterized by extensive deformation of the Earth's crust resulting from tectonic plate convergence, distinguished by the presence of folded and faulted rock formations, metamorphism, and igneous activity associated with mountain-building processes.

2.4K

Publications

184.7K

Citations

6.1K

Authors

1.2K

Institutions

Publications per year

2017–2026

589

Variants

OrogenesOrogenic Systems

Authors

6.1K

  1. MS
    Min Sun

    University of Hong Kong, Hong Kong SAR China

    47 publications · 6K citations

    33

    h-index

  2. WX
    Wenjiao Xiao

    Chinese Academy of Sciences, China

    48 publications · 6.8K citations

    33

    h-index

  3. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    40 publications · 4.9K citations

    31

    h-index

  4. GZ
    Guochun Zhao

    University of Hong Kong, Hong Kong SAR China

    30 publications · 3.8K citations

    24

    h-index

  5. SA
    Simon A. Wilde

    Curtin University, Australia

    24 publications · 5K citations

    23

    h-index

1–5 of 6.1K

Venues

  1. Geological Society London Special Publications

    104 publications · 13.7K citations

    53

    h-index

  2. Tectonics

    115 publications · 12.8K citations

    52

    h-index

  3. Tectonophysics

    111 publications · 10.2K citations

    52

    h-index

  4. Gondwana Research

    100 publications · 11.3K citations

    52

    h-index

  5. Precambrian Research

    105 publications · 7.8K citations

    50

    h-index

1–5