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《Journal of Jilin University(Earth Science Edition)》 2010-04
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Carbon and Oxygen Isotopic Composition and Its Genetic Significance in the Dajing Deposit,Inner Mongolia,China

WANG Chang-mingState Key Laboratory of Geological Processes and Mineral Resources/Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China  
Carbon and oxygen isotopic values provide criteria for the evaluation of depositional environment. Sixteen siderite samples from the Dajing ore deposit, Inner Mongolia, China, were analyzed in order to determine depositional environments. Siderites at the Dajing ore deposit are characterized by δ13CPDB from -1.8 ‰ to -6.6 ‰ and δ18OVPDB from -23.1 ‰ to -17.3 ‰, and their values lie in the hydrothermal sedimentary area on a δ13C versus δ18O diagram, showing hydrothermal sedimentary genesis of siderite. The palaeotemperature is estimated, based on the following equation: T=16.998-4.52(δ18cO-δ18wO) + 0.03(δ18cO-δ18wO)2. A higher palaeotemperature, averaging 117°C, suggests that the mineralizing fluids are from hydrothermal sedimentary fluids and deep lacustrine water. Depositional settings of limestone can be inferred from equation: Z=2.048(δ13C+50)+0.498(δ18O+50). Samples with Z value above 120 would be classified as marine, while those with Z below 120 as fresh-water ones. The synthetic Z parameter (between 100 and 114) in the Dajing ore deposit, also suggests lacustrine environments. Together with tectonic setting, deposit geology, and rare-earth element composition, the hydrothermal systems are recognized in a lacustrine setting in the early mineralization, which is important not only for a better understanding and interpretation of the genesis of the Dajing deposit but also for exploration of hydrothermal events in the lacustrine environment.
【Fund】: 国家“973”计划项目(2009CB421008);; 教育部长江学者和创新团队项目(IRT0755);; “111”计划项目(B07011);; 中国博士后基金项目(20090460400)
【CateGory Index】: P618.13
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6 SHAO Jun1, 2,WANG Shicheng1,MA Xiaolong3,FU Xiuyou4ZHANG Jiongfei2,ZHAO Zhenyu1,ZHU Hongchen2(1.Institute of Mineral Resources Prognosis of Synthetic Information, Jilin University, Changchun130026,China;2. Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang110032,China;3. General Institute of Mineral Prospect and Development, Qiqihaer161006,China;4. Zhalantun Bureau of Land and Resources, Zhalantun162050,China);REGIONAL METALLOGNETIC CHARACTERISTICS OF GOLD AND MULTIMETAL DEPOSITS IN NORTHERN DAXING'ANLING MOUNTAIN[J];Journal of Changchun University of Science and Technology;2003-01
7 ZHU Hong-chen,ZHANG Jiong-fei,QUAN Heng (Shenyang Institute of Geology and Mineral Resources, Shenyang110032, China);Two Stages of Mesozoic Lithogenesis and Mineralization in Daxing'anling Mountains[J];Journal of Jiling University (Earth Science Edition);2005-04
8 Xia Jun Li Xiuhua Wang Chengshan Zhao Wanli Cheng Xueru;CHARACTERISTICS OF MESOZOIC VOLCANIC ROCKS IN HAILAER AND ITS ADJACENT AREAS AND DISCUSSION ON VOLCANIC ROCKS OF MARGINAL BLOCK TYPE[J];;1993-04
9 ZHENG Rong cai 1, WANG Cheng shan 1, ZHU Li dong 1, LIU Hong jun 1, FANG Guo yu 2, DU Wen bo 2, WANG Chong xiao 2, WANG Man fu 2 (1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, China; 2.Research Institute of Yumen Oil Field Branch Company);DISCOVERY OF THE FIRST EXAMPLE OF "WHITE SMOKE TYPE" OF EXHALATIVE ROCK (HYDROTHERMAL SEDIMENTARY DOLOSTONE) IN JIUXI BASIN AND ITS SIGNIFICANCE[J];Journal of Chengdu University of Technology(Science & Technology Edition);2003-01
10 ZHANG Shouting1, ZHAO Pengda1, CHEN Jianping1, XU Zhanzhang2(1.China University of Geosciences, Beijing; 2.Chengdu University of Technology, China);MULTITARGET MINERALS PREDICTION AND ASSESSMENT AND THEIR SIGNIFICANCE[J];Journal of Chengdu University of Technology(Science & Technology Edition);2003-05
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