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WANG Zongxiu, LI Tao. 2004: Mechanism of Cenozoic revival orogeny in the Bogda mountain chain, Xinjiang. Geological Bulletin of China, 23(3): 286-293. DOI: 10.12097/gbc.20040347
Citation: WANG Zongxiu, LI Tao. 2004: Mechanism of Cenozoic revival orogeny in the Bogda mountain chain, Xinjiang. Geological Bulletin of China, 23(3): 286-293. DOI: 10.12097/gbc.20040347
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Mechanism of Cenozoic revival orogeny in the Bogda mountain chain, Xinjiang

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  • Revised Date: September 04, 2003
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  • The Bogda mountain chain grew in the Cenozoic.Its evolution went through a complete pro-cess,i.e.Paleozoic initial orogeny,Mesozoic extension and readjustment and Cenozoic revival orogeny.The Bogda mountain chain is an ideal area for the study of intracon
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