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
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
Mechanism of Cenozoic revival orogeny in the Bogda mountain chain, Xinjiang
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