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《Geotectonica Et Metallogenia》 2009-02
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Cenozoic Tectonic Rotation of the Liupan Shan Region in the Northeastern Tibetan Plateau and Its Implications

LIU Yongqian1,FANG Xiaomin1,2,SONG Chunhui2,LI Lili2 and CHENG Yu2(1.Center for Basin Resource and Environment,Institute of Tibetan Plateau Research,CAS,Beijing 100085,China;2.MOE Key Laboratory of Western China's Environmental Systems,College of Resources and Environment Sciences,Lanzhou University,Lanzhou 730000,Gansu,China)  
The Liupan Shan region is located at the northeastern-most corner of the Tibetan Plateau in tectonics.A series of southward-arced sinistral faults(Haiyuan-Liupan Shan Fault,Xiang Shan-Tianjing Shan Fault,Yantong Shan-Yao Shan Fault and Qingtongxia-Guyuan Fault) control the formation and distribution of inter-fault blocks and basins,in which thick Cenozoic sediments were deposited.Knowledge of the evolution and deformation of this region will enhance our understanding of the mechanisms of the Tibetan growth and its influence on global climate change.High-resolution paleomagnetic study of the Dingjiaergou section,5 km north of Tongxin County,Ningxia Hui-autonomous Region shows a total 23° clockwise tectonic rotation of the Liupan Shan region from the Cretaceous to the Mid-Miocene,manifesting three intervals of fast rotations in 33~30Ma at 9±2.6°,in 30~23 Ma at 9±3.5° and in 23~16 Ma at 5±3.7°.These rotations are accordant with some unconformities or sedimentary environmental rapid changes.All these indicate that the deformation frontier from the India-Eurasia collision had reached the Liupan Shan region at least about Late Eocene to the Early Oligocene,which is almost 30 million years earlier than the current general view that the deformation and uplift of the Liupan Shan had begun since the Quaternary.
【Fund】: 中国科学院知识创新工程重要方向项目(编号:KZCX2-YW-104);; 国家教育部科学技术研究重大项目(编号:306016);; 国家973重点基础研究发展计划项目(2005CB422001)的联合资助
【CateGory Index】: P542
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