Orogenic Plateau Formation is a geological process denoting the tectonically driven uplift and broad crustal thickening of continental lithosphere, distinguished from other orogenic features by the development of a high-elevation, low-relief topographic plateau as a direct consequence of compressional stress and crustal shortening in collisional mountain belts.
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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
The origin and pre-Cenozoic evolution of the Tibetan Plateau
Di‐Cheng Zhu, Zhidan Zhao, Yaoling Niu et al. · Gondwana Research · 2012 · 1.3K citations · Full text
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Chinese Academy of Sciences
Beijing, China
71 h-index
486 publications
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Institute of Geology and Geophysics
Beijing, China
57 h-index
283 publications
29.3K citations
Chinese Academy of Geological Sciences
Beijing, China
51 h-index
348 publications
34K citations
China University of Geosciences (Beijing)
Beijing, China
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173 publications
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Northwest University
Xi'an, China
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China University of Geosciences
Wuhan, China
38 h-index
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Centre National de la Recherche Scientifique
Paris, France
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166 publications
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Peking University
Beijing, China
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