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《Geology in China》 2006-02
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Deformation and tectonic evolution of the Karakorum fault, western Tibet

LI Hai-bing, Franck Valli, XU Zhi-qin, YANG Jing-sui,Paul Tapponnier, Robin Lacassin, CHEN Song-yong, QI Xue-xiang, Marie-Luce Chevalier (Key Laboratory of Continental Dynamics, MLR,Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China; Department of Earth Sciences, University of Hong Kong, Hong Kong S.A.R. China; Institut de Physique du Globe de Paris, 75252 Paris, France)  
The deformation features, age, tectonic evolution and tectonic role of the Karakorum fault (KF) have long been controversial. In the Ayila Ri'gyii area in the southeastern segment of the KF, dextral sheared mylonite and mylonitized gneiss-granite are exposed along the fault. Microstructural study indicates high-temperature, dextral shear features, accompanied by the generation of synkinematic leucogranite. The U-Pb ages recorded by synkinematic crystalline zircons imply that:the KF formed at least before 23-25 Ma and its continuous deformation at least continued to -12 Ma, when the deformation was accompanied by rapid uplift of the Ayila Ri'gyu Range and initiation of the Gar basin. Integrated analysis indicates that the growth process of the KF might be a process of northwest-directed propagation and the result of continuous India-Eurasia collision. The cumulative displacement amount is at least 280 km along the fault, and an average long-term slip rate is -11 mm/a on the fault. Rigid block kinematic analysis suggests that material of the Qinghai-Tibet Plateau was extruded toward -108° at a rate of 16.2 mm/a after -23-25 Ma.
【Fund】: 国土资源部科技司青藏高原专项课胚(2001010201) 国家自然科学基金项目(40272096)资助
【CateGory Index】: P542.3
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