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《Journal of Glaciology and Geocryology》 2012-03
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Feathery Faults Formation in Kumtagh Desert: Bayiquan Tectonic Movement and Its Relationship among Qinghai-Tibet Plateau Uplift and Climate Change

ZHENG Ben-xing1,QU Jian-jun1,2,3,SHEN Yong-ping1,NIU Qing-he1,2,3, YU Qi-hao1,ZHAO Ai-guo1(1.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China; 2.Dunhuang Gobi and Desert Research Station,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China;3.Gansu Center for Sand Hazard Reduction Engineering and Technology,Lanzhou Gansu 730000,China)  
In this article,the author discuss the relationship between the formation of feathery faults in Kumtagh Desert and Baiyiquan tectonic movement,and modify the Pliocene strata of previous research to deformation strata of late stage of middle Pleistocene,it's also the evidence of Baiyiquan tectonic movement(227 ka BP).The particular stage during the Qinghai-Tibet Plateau uplift and the influence to climate change in north of Plateau are also discussed.We establish the sequence relationship between Qinghai-Tibet Plateau uplift and climate change.
【Fund】: 国家自然科学基金重点项目(40930741);; 全球变化研究国家重大科学研究计划项目(2010CB951404);; 中国科学院知识创新方向性项目(KZCX2-YW-329)资助
【CateGory Index】: P542.3
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