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
Parents
515
1–5 of 515
1.4K
13
h-index
13
h-index
12
h-index
University of California, Los Angeles, United States
11 publications · 2.1K citations
11
h-index
10
h-index
1–5 of 1.4K
461

Chinese Academy of Geological Sciences
Beijing, China
26 h-index
144 publications
13.7K citations

Chinese Academy of Sciences
Beijing, China
23 h-index
111 publications
6.4K citations

Wadia Institute of Himalayan Geology
Dehra Dūn, India
20 h-index
56 publications
2.3K citations

China University of Geosciences (Beijing)
Beijing, China
18 h-index
47 publications
2.2K citations
China University of Geosciences
Wuhan, China
17 h-index
45 publications
2.5K citations

Centre National de la Recherche Scientifique
Paris, France
16 h-index
52 publications
5.5K citations
Institute of Geology and Geophysics
Beijing, China
16 h-index
60 publications
4.6K citations
University of California, Los Angeles
Los Angeles, United States
15 h-index
41 publications
7.3K citations
1–8 of 461
42 publications · 6.2K citations
37
h-index
35 publications · 5.6K citations
31
h-index
44 publications · 3.8K citations
30
h-index
22 publications · 3.9K citations
21
h-index
25 publications · 1.4K citations
20
h-index
1–5