Himalayan-type Orogeny

Himalayan-Type Orogeny is a continental collisional orogeny characterized by the intense crustal shortening, thickening, and uplift resulting from the ongoing convergence between the Indian and Eurasian plates, forming high-grade metamorphic belts, extensive thrust systems, and a doubly vergent mountain belt without significant arc magmatism.

515

Publications

43.4K

Citations

1.4K

Authors

461

Institutions

Publications per year

2017–2026

119

Variants

Himalayan-style Orogeny

Authors

1.4K

  1. MP
    M. P. Searle

    University of Oxford, United Kingdom

    13 publications · 1.1K citations

    13

    h-index

  2. PJ
    Peter J. Treloar

    Kingston University, United Kingdom

    14 publications · 930 citations

    13

    h-index

  3. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    12 publications · 1.1K citations

    12

    h-index

  4. TM
    T. Mark Harrison

    University of California, Los Angeles, United States

    11 publications · 2.1K citations

    11

    h-index

  5. JZ
    Jinjiang Zhang

    Peking University, China

    10 publications · 599 citations

    10

    h-index

1–5 of 1.4K

Venues

  1. Geology

    42 publications · 6.2K citations

    37

    h-index

  2. Earth and Planetary Science Letters

    35 publications · 5.6K citations

    31

    h-index

  3. Tectonophysics

    44 publications · 3.8K citations

    30

    h-index

  4. Geological Society of America Bulletin

    22 publications · 3.9K citations

    21

    h-index

  5. Journal of Asian Earth Sciences

    25 publications · 1.4K citations

    20

    h-index

1–5