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《Geology of Anhui》 2001-03
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STUDY ON THE STRUCTURAL FEATURES OF THE HUANGLISHU-MIAOJI FAULT ZONE

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 Anhui Province, Hefe  
The Huanglishu Miaoji Fault Zone is an important part of the root of the Chuzhou Chaohu foreland fold thrust belt at the northeast fringe of the Yangtze landmass. It is characterized by developed ductile and brittle ductile shear zones whose deformation mechanism is of simple shear. Major faulting took place under the condition of 150 MPa for differential stress and 8×10-16/s for strain rate. The fault has been subjected to three stages such as thrusting, right handed strike slipping and normal rifting. The fractal values for the northern part are higher than those for the southern part of the middle section of the fault zone. The discovery of the Yangtze type Neoarchean metamorphic basement to the west side of the fault zone and the coincidence of the Yenshanian intermediate acid intrusive isotope geochemical characteristics for both sides of it suggested that the Huanglishu-Miaoji Fault Zone is not the boundary between the Dabie orogen and the Yangtze landmass.
【Fund】: 原地质矿产部“安徽新类型、新地区、新矿种找矿研究”项目(编号地科专96-06)的部分研究成果
【CateGory Index】: P542
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