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《Earth Science Frontiers》 2004-04
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Geochronology of the dextral strike ductile shear zone in south margin of the Northern Qilian Mountains and its geological significance

QI Xue-xiang~1, ZHANG Jian-xin~1, LI Hai-bing~1, CAI Jin-lang~2 (1. Laboratory of Continental Dynamics, Institute of Geology, CAGS, Beijing 100037, China; 2. Department of Earth Sciences, Cheng-Kung University, Tainan, Taiwan, China)  
The dextral strike-slip ductile shear zone in the northern Qilian Mountains is located at the boundary between Qilian terrane and north Qilian Caledonian subduction-collision complex belt. It is about 800 km long, 5 to 6 km wide, striking NWW-SEE and dipping north. The dextral strike slipping and transpressive deformation are revealed by the senses of shear and the stretching lineations plunging low-angled to SE. The upper intersection age for single zircon U-Pb isotopic isochrone with TIMS method is 965~956 Ma, which represents the metamorphic age of the metamorphic rock of basement in Qilian block. The results of~(40)Ar/~(39)Ar age dating to the K-feldspar and biotite from mylonites, and the relationships among ductile shear zone, strata and intrusions indicate that the ductile shear zone formed between 440 and 380 Ma. The dextral strike-slip ductile shear zone in south margin of north Qilian Mountains was formed by a large-scale transpression resulted from the continent-continent oblique collision between Qilian block and Alxa block in Qilian Caledonian orogeny.
【Fund】: 973专项项目(200313000058);; 国家自然科学基金资助项目(40272096);; 中国地质调查局地质调查项目(200313000058)
【CateGory Index】: P597.3
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【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 ZHANG Jian-xin, YANG Jing-sui, XU Zhi-qin, ZHANG Ze-ming, CHEN Wen, LI Hai-bing (Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China);Peak and retrograde age of eclogites at the northern margin of Qaidam basin, northwestern China: Evidences from U-Ph and Ar-Ar datas[J];GEOCHIMICA;2000-03
2 Liu Jichen (China University of Geosciences, Wuhan 430074);TECTONICS OF CONTINENTAL BLOCK IN NORTH QILIAN OROGENIC BELT[J];;1991-06
3 LEE CHUN-YU (Geological Institute of Northwest China);TECTONIC EVOLUTIONS OF SOME MOUNTAIN RANGES IN CHINA, AS TENTATIVELY INTERPRETED ON THE CONCEPT OF PLATE TECTONICS[J];Chinese Journal of Sinica;1975-01
4 LIU XUN;FU DE-RONG;WEI GUANG-MING;WANG YONG (Institute of Geology ,Chinese Academy of Geological Sciences,Beijing100037);TECTONIC EVOLUTION OF TERRANES IN THE CORRIDOR OF GOLMUD-EJIN QI GEOTRANSECT BY STUDY ON THE SEDIMENTARY FEATURES[J];Chinese Journal of Geophysics;1995-S2
5 Xie Zhi 1) Chen Jiangfeng 1) Dong Shuwen 2) Li Huimin 3) Zhou Taixi 1) Zuo Yicheng 3) Zhou Hongying 3) ( 1) Department of Earth and Space Sciences,University of Science and Technology of China,Hefei; 2)Chinese Ac;The Zircon U-Pb Ages of the Low-grade Metamorphic Rocks in the Southern Part of Dabie Mountain,China[J];;1999-04
6 Zhang Jianxin xu Zhiqing(Institute of Geology,CAGS,Beijing);Caledonian Subduction-Accretionary Conplec/Volcanic Arc Zone and Its Deformation Features in the Middle Sector of North Qilian Mountains[J];;1995-02
7 Xia Zuchun; Xia Linqi; Xu Xueyi (Xi'an Institute of Geology and Mineral Resources,CAGS);The Late-Proterozoic-Cambrian Active Continental Rift Volcanism in Northern Qilian Mountains[J];;1996-03
8 FENG Yimin (Xi′an Institute of Geology and Mineral Resources,CAGS,Xi′an 710054);INVESTIGATORY SUMMARY OF THE QILIAN OROGENIC BELT,CHINA:HISTORY, PRESENCE AND PROSPECT[J];ADVENCE IN EARTH SCIENCES;1997-04
9 ZUO Guochao (Institute of Geoscience, Gansu Bureau of Geology and Mineral Resources, Lanzhou 730000) WU Hanquan (Xi'an Institute of Geology and Mineral Resources, Xi'an 710054);A BISUBDUCTION COLLISION OROGENIC MODEL OF EARLY PALEOZOIC IN THE MIDDLE PART OF NORTH QILIAN AREA[J];ADVENCE IN EARTH SCIENCES;1997-04
10 ZHANG Qi ①, SUN Xiaomeng ②, ZHOU Dejin ① QIAN Qing ①, CHEN Yu③, WANG Yueming ④ JIA Xiuqin ⑤, HAN Song ⑤ (①Institute of Geology, Chinese Academy of Sciences, Beijing 100029;②Engineering and Technology College, Science and Techn;THE CHARACTERISTICS OF NORTH QILIAN OPHIOLITES, FORMING SETTINGS AND THEIR TECTONIC SIGNIFICANCE[J];ADVENCE IN EARTH SCIENCES;1997-04
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