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《Geotectonica Et Metallogenia》 2006-04
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NEOTECTONICS IN SOUTHERN YILI BASIN AND ITS CONTROL OF SANDSTONE-TYPE URANIUM DEPOSITS

WANG Yong1, CHEN Zhengle2, LIU Jian2, ZHENG Enjiu3, WANG Cheng3, LI Shengxiang4 and HAN Xiaozhong4 (1. Institute of Mineral and Resources, CAGS, Beijing 100037, China; 2. Institute of Geomechanics, CAGS, Beijing 100081, China; 3. No. 216 Geological Party, Bureau of Geology of CNNC, Urumqi, Xinjiang 830011, China; 4. Beijing Research Institute of Uranium Geology, Beijing 100029, China)  
Research of the neotectonic activities forms an important part of the research of the uranium mineralization in the Yili basin. In this paper the characteristics of the neotectonic activities and the neotectonic control of the uranium mineralization in the Yili basin are studied, the basic characters of the neotectonic activities are described, the neotectonic scratches and joints are statistically analyzed and the neotectonic activities are dated by using the ESR technique. The analytical results show that the neotectonic activities resulted from the nearly north-south-trending compressional stress in the region. Based on previous research results, the neotectonic activities in this area can be divided into five evolution stages: late Eocene to Oligocene, Miocene, late Pliocene to early Pleistocene, early Pleistocene to Mid-Pleistocene, and Mid-Pleistocene to now. Our research demonstrates that the sandstone-type uranium mineralization is closely related to the neotectonic activities, and that the neotectonic activities control the distribution of the sandstone type uranium deposits, and especially the east-west-trending faults. Based on the characteristics of the neotectonic activities, it can be concluded that the ore-forming conditions and hence the prospecting perspective in the west part are better than those in the east part.
【Fund】: 国家重点基础研究发展规划(973)项目(课题编号:2001CB409808)资助.
【CateGory Index】: P619.14
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