Accretionary Orogens
Accretionary Orogens is a tectonic model of mountain building characterized by the gradual growth of continental crust through the accretion of oceanic and continental terranes at convergent plate margins, distinguishing it from collisional orogens that form primarily by continent-continent convergence.
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Tectonic models for accretion of the Central Asian Orogenic Belt
Brian F. Windley, D. V. Alexeiev, Wenjiao Xiao et al. · Journal of the Geological Society · 2006 · 3.4K citations · Full text
Review of global 2.1–1.8 Ga orogens: implications for a pre-Rodinia supercontinent
Guochun Zhao, Peter A. Cawood, Simon A. Wilde et al. · Earth-Science Reviews · 2002 · 1.6K citations
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Chinese Academy of Sciences
Beijing, China
63 h-index
414 publications
69.7K citations
Institute of Geology and Geophysics
Beijing, China
52 h-index
254 publications
51.1K citations
Curtin University
Perth, Australia
41 h-index
66 publications
10.8K citations

Chinese Academy of Geological Sciences
Beijing, China
38 h-index
178 publications
23.3K citations

University of Hong Kong
Pok Fu Lam, Hong Kong
36 h-index
112 publications
24.9K citations

University of Leicester
Leicester, United Kingdom
34 h-index
54 publications
17.4K citations

Centre National de la Recherche Scientifique
Paris, France
32 h-index
106 publications
10.4K citations
Guangzhou Institute of Geochemistry
Guangzhou, China
30 h-index
109 publications
14K citations
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