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《Mineral Deposits》 2015-01
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Geochemistry and geochronology of ore-bearing granites in Suyunhe Mo deposit,West Junggar, Xinjiang

ZHONG ShiHua;SHEN Ping;PAN HongDi;ZHENG GuoPing;YAN YuHong;LI Jing;Key Laboratory of Mineral Resources, Institute of Geology and Geophysics,Chinese Academy of Sciences;University of Chinese Academy of Sciences;College of Earth Sciences, Chang'an University;No. 1 Regional Geological Survey Party of Xinjiang Bureau of Geology and Mineral Exploration and Development;Hebei United University;  
The Suyunhe Mo deposit, located in western Barluk Mountain of West Junggar Basin, consists of three granitic stocks. These granites share similar geochemical features. They are characterized by high content of Rb, Th, U,LREE, and relatively negative anomalies of Ba, P, Ti, suggesting I-type granites. Data from some samples indicate that the granites have undergone fractional crystallisation. The results of LA-ICPMS zircon U-Pb dating indicate that the magmatism in the Suyunhe Mo deposit occurred in Late Carboniferous( 309. 3 ~ 310. 2 Ma), which was related to the Mo mineralization. The biotite Ti thermometry suggests that the crystal temperatures of stock Ⅰ and Ⅲ are704 ~ 739℃, whereas the crystal temperatures of stock Ⅱ( 659 ~ 681℃) are lower. Meanwhile, the amphiboleplagioclase barometer indicates that the pressures of stock Ⅰ and Ⅲ are( 3. 0 ~ 3. 9) × 108 Pa. Both mineral chemistry and petrogenesis studies suggest that the three stocks formed in an island-arc setting. In addition, the Barluk metallogenic belt, represented by the Suyunhe Mo deposit, is similar to Balkhash metallogenic belt in geochemistry and geochoronology, suggesting that the Balkhash metallogenic belt probably extends eastward to the Barluk metallogenic belt.
【Fund】: 中国科学院知识创新工程项目(编号:KJZD-EW-TZ-G07-1);; 国家自然科学基金项目(编号:U1303293 41390441 41272109);; 国家科技支撑计划305项目(编号:2011BAB06B01)的联合资助
【CateGory Index】: P618.65;P597.3
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