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《Geology in China》 2010-02
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The Permian lithofacies paleogeographic characteristics and basin-mountain conversion in the Kunlun orogenic belt

CHEN Shou-jian1, LI Rong-she1, JI Wen-hua1, ZHAO Zhen-ming1, LIU Rong-li1, JIA Bao-hua2, ZHANG Zhen-Fu3, WANG Guo-can4 (1. Xi’an Institute of Geology and Mineral Resources, Xi’an 710054, Shaanxi, China; 2.Hunan Institute of Geological Survey, Changsha 410011, Hunan, China;3.Shanxi Institute of Geological Survey, Taiyuan 030001, Shanxi, China;4.China University of Geosciences, Wuhan 430074, Hubei, China)  
The Kunlun orogenic belt was basically formed in Paleozoic, resulting from ocean-continent conversion and collision orogenic activity. In the early and middle Permian, the south Kunlun was a multi-island ocean basin, the north Kunlun was an active margin rift and contained mainly shallow sea sediments and partly volcanic basin sediments, the middle part was a seashore -shallow sea, and the Kangxiwa -Muztagh-Animaqing belt contained deep-semi-deep sediments and formed a multi-island ocean basin paleogeographic framework in this period. In the middle and late Permian, convergence took place, ocean basin and active margin rift were closed, uplifting began, and basin-mountain conversion was completed. In the late Permian, the Kunlun orogenic belt entered into another basin-mountain conversion period, sea water came from southeast in the east part and from northwest in the west part, with the deposition of seashore-shallow sea fragmental rocks and carbonate rocks in local areas. Based on field work, analytical tests and integrated studies in association with the 1:250 000 regional geological data and other data available, the authors chose the Permian strata of late Palaeozoic as the study object and discussed the Permian lithofacies characteristics and tectono-paleogeography with the purpose of improving the research level of the Kunlun orogenic belt.
【Fund】: 中国地质调查局重点项目“青藏高原北部空白区基础地质调查与研究”(1212010310101);; “青藏高原前寒武纪地质古生代构造-古地理研究”(1212010610102);; 国家自然科学基金(40872084)联合资助
【CateGory Index】: P531
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10 YANG Jie;PEI Xian-zhi;LI Rui-bao;LI Zuo-chen;LIU Zhan-qing;PEI Lei;LIU Cheng-jun;CHEN You-xin;CHEN Guo-chao;GAO Jing-min;College of Earth Science and Resources,Chang'an University;Key Laboratory of Western China's Mineral Resources and Geological Engineering,Ministry of Education;College of Earth Science,Guilin University of Technology;School of Earth Sciences and Resources,China University of Geosciences;;Geochemical characteristics and geological implications of Haerguole basalt in Buqingshan area on the southern margin of East Kunlun Mountains[J];Geology in China;2014-02
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