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《Geotectonica Et Metallogenia》 2005-04
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SEDIMENT-STRUCTURAL EVOLUTION AND LEAD-ZINC MINERALIZATION IN THE DEVONIAN VOLCANO-SEDIMENTARY KELAN BASIN IN SOUTHERN ALTAY, XINJIANG

YIN Yiqiu1, YANG Youming2, LI Jiaxing2, GUO Zhenglin3 and GUO Xuji3 (1. Guilin Research Institute of Geology and Mineral Resources, Guilin, Guangxi 541004, China; 2. Xinjiang Bureau of Geological Exploration for Nonferrous Metal Resources, Urumqi, Xinjiang 830000, China; 3. No.706 Geological Party, Xinjiang Nonferrous Metal Geoexploration Bureau, Aletai, Xinjiang 836500, China)  
Located in the Altay edge of the Siberia plate, the Kelan Basin is obviously an asymmetric Devonian volcano-sedimentary basin, its sediment-structural evolution may be divided into three stages: the early acidic volcano-sedimentary stage, the middle base volcano-sedimentary stage and the late clastic sedimentary stage. Mineralization occurred in the stages of the structural evolution, resulting in the corresponding deposit types. The VHMS lead-zinc mineralization occurred in the early acidic volcano-sedimentary stage, and corresponds to the acidic volcanic eruption. The SEDEX lead-zinc mineralization occurred in the middle base volcano-sedimentary stage, and corresponds to the base volcanic eruption. The extremely poor mineralization occurred in the late clastic sedimentary stage, and corresponds to the sedimentation process of the terrigenous clastics.
【Fund】: 国家305项目[“十五”重点科技攻关项目(2001BA609A-07)];; 新疆维吾尔自治区资源补偿费项目(编号:2003005);; 广西培养新世纪学术和技术带头人专项资金项目(编号:2002204)共同资助.
【CateGory Index】: P618.42;
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