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《Earth Science Frontiers》 2008-03
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Sinistral transpressive deformation in the northern part of Zhangbaling uplift in the Tan-Lu fault zone and its ~(40)Ar/~(39)Ar dating.

Zhang Qing1, Zhu Guang2, Liu Guosheng2 , C.Teyssier1, W.J.Dunlap3 1.Department of Geology and Geophysics, University of Minnesota, Minneapolis MN55455, USA2.College of Resource and Environment Engineering, Hefei University of Technology, Hefei 230009, China3.Research School of Earth Sciences, Australian National University, Acton, ACT 0200,Australia  
Ductile detachment deformation belt, brittle-ductile transition belt and brittle foreland fold-fault belt are exposed on the northern part of Zhangbaling uplift in the Tan-Lu fault zone from west to east. The Zhangbaling schists in the ductile detachment deformation belt are widely mylonitized under low greenschist facies. The belt shows gentle mylonitic foliation and nearly N-S trending mineral elongation lineation. Analyses of microstructures and quartz C-axis fabrics demonstrate that the ductile detachment belt has experienced top-to-south motion. The deformation motion changes into top-to-SSE then top-to-SE thrusting, showing a sinistral transpressive deformation zone. The ductile deformation belt exposed in the Zhangbaling group is a detachment deformation belt between deeper, steep strike-slip structures and shallower, brittle structures. The differential deformation between the different levels caused top-to-south shear motion under a general northward movement of the fault block. 40Ar/39Ar dating of muscovite separated from the Zhangbaling schists with different grain sizes indicates that the deformation took place in a range from (236.2±0.5) Ma to (238.0±0.4) Ma, i.e. the latest Middle Triassic. It is suggested that the sinistral displacement of the Tan-Lu fault zone happened in a continental, deep subduction stage of the North and South China plate collision, and was derived from intracontinental transform faulting.
【Fund】: 国家自然科学基金资助项目(40272094 40672131 90714004)
【CateGory Index】: P542
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6 ZHU Guang (Hefei University of Technology, Hefei,230009);GEOTECTONIC IMPLICATIONS OF THE DEFORMATION AND METAMORPHISM OF THE PENGLAI GROUP OF THE JIAOBEI REGION, CHINA[J];Geotectonica Et Metallogenia;1993-03
7 TU Yin jiu 1, LIU Xiang pei 2, WANG Xiang yun 3, WU Ming an 4 (1. No.312 Geological Party of Anhui Province, Bengbu 233040, China; 2. Anhui Bureau of Geology and Mineral Resources, Hefei 230001, China; 3. NO.327 Geological Party of;STUDY ON THE CHUZHOU CHAOHU FORELAND FOLD THRUST ZONE AT THE NORTHERN MARGIN OF THE LOWER YANGTZE LANDMASS[J];Geotectonica Et Metallogenia;2001-01
8 WU Yue-dong,JIANG Lai-li,CHU Dong-ru,WU Wei-ping,WU Hai-quan,WANG De-hua(Anhui Institute of Geological Survey,Hefei230001,Anhui,China);Basin-Range coupling between the Dabie orogen and the Meso-Cenozoic basins along the Yangtze River in Anhui Province[J];Chinese Geology;2003-03
9 HOU Ming-jin1,2, WU Yue-dong2, TANG Jia-fu2(1.School of Resources and Environment Engineering, Hefei University of Technology,Hefei 230009, Anhui, China;2. Anhui Geological Survey, Hefei 230001, Anhui, China);Deformation features of the mid-upper crust of the Dabie orogenic belt-a case study of the Indosinian-early Yanshanian tectonic deformation in the Zhangbaling area[J];Chinese Geology;2004-02
10 LIU Yi- can1,2, LI Shu- guang1, XU Shu- tong2, JAHN Bor- Ming3, ZHENG Yong- fei1, ZHANG Zong- qing4, JIANG Lai- li2, CHEN Guan- bao2, WU Wei- ping2 (1. Department of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026,;Sm-Nd dating of eclogites from Northern Dabie Mountains and its constraints on the timing of granulite- facies retrogression[J];Geochimica;2001-01
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