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  5. Haerguole Ophiolite in the Buqingshan Tectonic Mélange Belt, Northern Qing-Tibet Plateau, China: Rel

Haerguole Ophiolite in the Buqingshan Tectonic Mélange Belt, Northern Qing-Tibet Plateau, China: Rel

来源 :The International Conference on Continental Dynamics(2014年大陆 | 被引量 : 0次 | 上传用户：czh126
【摘 要】
：
Buqingshan tectonic mélange belt (BTMB)is located in the Buqingshan-Manite area,southern margin of East Kunlun Orogenic Belt (EKOB),Central Orogenic Belt (COB) of Chnia,geographically.It is bounded by
【作 者】
：
Xianzhi Pei Ruibao Li Guochao Chen Chengjun Liu Youxin CHEN Zuochen Li Tong Xu Xiaobin Li 
【机 构】
：
Key Laboratory of Western China's Mineral Resources and Geological Engineering,Ministry of Educatio
【出 处】
：
The International Conference on Continental Dynamics(2014年大陆
【发表日期】
：
2014年5期
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论文部分内容阅读
Buqingshan tectonic mélange belt (BTMB)is located in the Buqingshan-Manite area,southern margin of East Kunlun Orogenic Belt (EKOB),Central Orogenic Belt (COB) of Chnia,geographically.It is bounded by the EKOB to the north and the Hoh Xil-Bayan Har orogenic belt to the south.To the east,it is joined with the Anemaqen tectonic belt.This belt extends in an E-W direction,with a width of 10 km and a length of 35 km,recording some important continent-ocean evolution information concerning the Tethyan Ocean.BTMB comprises different types of tectonic mélange blocks outcropped in lenticular shape and Permian turbidite deformed strongly.
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