Andean-type Orogeny
Andean-Type Orogeny is a tectonic process characterized by mountain building at convergent plate boundaries where oceanic lithosphere subducts beneath continental lithosphere, resulting in crustal thickening, magmatic arc development, and uplift without significant continent-continent collision.
655
Publications
54.4K
Citations
2.1K
Authors
643
Institutions
Publications per year
2017–2026
127
Variants
Andean-style Orogeny
Parents
655
Alwyn H. Gentry · Annals of the Missouri Botanical Garden · 1982 · 923 citations · Full text
Andean tectonics as a cause for changing drainage patterns in Miocene northern South America
Carina Hoorn, Javier Guerrero, Gustavo Sarmiento et al. · Geology · 1995 · 677 citations
Tectonics and history of the Andaman Sea region
Joseph R. Curray · Journal of Asian Earth Sciences · 2005 · 645 citations
1–5 of 655
2.1K
11
h-index
9
h-index
7
h-index
6
h-index
6
h-index
1–5 of 2.1K
643

Centre National de la Recherche Scientifique
Paris, France
33 h-index
98 publications
11K citations

Consejo Nacional de Investigaciones Científicas y Técnicas
Buenos Aires, Argentina
25 h-index
113 publications
4.4K citations
Universidad de Buenos Aires
Buenos Aires, Argentina
23 h-index
77 publications
5.2K citations

Chinese Academy of Sciences
Beijing, China
23 h-index
88 publications
6.3K citations
University of Chile
Santiago, Chile
19 h-index
43 publications
3.2K citations

Chinese Academy of Geological Sciences
Beijing, China
19 h-index
69 publications
9.1K citations
Institute of Geology and Geophysics
Beijing, China
18 h-index
58 publications
3.9K citations

Australian National University
Canberra, Australia
16 h-index
19 publications
2.3K citations
1–8 of 643
67 publications · 7K citations
43
h-index
55 publications · 4.8K citations
40
h-index
42 publications · 4.1K citations
34
h-index
38 publications · 4.6K citations
31
h-index
35 publications · 5K citations
30
h-index
1–5