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《Acta Geologica Sinica》 2004-01
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Molybdenite Re-Os Precise Dating for Molybdenite from Cu-Au-Mo Deposits in the Middle-Lower Reaches of Yangtze River Belt and Its Implications for Mineralization

MAO Jingwen1,2) ,Holly STEIN3) ,DU Andao4),ZHOU Taofa5) ,MEI Yanxiong1), LI Yongfeng1), ZANG Wenshuan2),LI Jinwen1,2) 1) Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037 2) Faculty of Geosciences and Resources, China University of Geosciences, Beijing, 100083 3) AIRIE Program, Department of Earth Resources, Colorado State University, Fort Collins, USA 4) National Research Center of Geoanalysis, Chinese Academy of Geological Sciences, Beijing, 100037 5) Department of Resource and Environmental Sciences, Hefei University of Technology, Hefei, 230009  
The Middle-Lower Yangtze River metallogenic belt is an important corridor for Cu-Au-Mo-Fe deposits in East China. Because there are porphyry-skarn Cu-Au-Mo deposits, and stratabound Cu-Au-Mo deposits, their origin have been strongly controversial for a long time. We obtained eleven molybdenite samples from five skarn-porphyry Cu-Au-Mo deposits and the other five samples from the Datuanshan stratabound Cu-Au-Mo deposit for Re-Os dating. The total 16 samples are dated with ICP-MS method and 9 of them are dated by NTIMS. The results from the two methods of ICP-MS and NTIMS are almost concordant each other. Re-Os model ages of 16 molybdenite range from 134. 7±2. 3 to 143. 7±1. 6Ma (2σ) in which the model ages of the five samples from the Datuanshan deposit are quite close, varying from ?38. 0±3. 2 to 140. 8±2. 0 Ma, averaging 139. 3±2. 6 Ma, their corresponding isochron is 139. l±2. 7 Ma with initial Os value of 0. 7±8.1 (MSDW =0. 29). These data definitely reflect the porphyry-skarn-Cu-Au-Fe-Mo deposits and the stratabound skarn Cu-Au-Mo deposits share the same forming ages and are the products of a same metallogenic system. They all occurred at the time of the transition stage of geodynamic regimes i. e. from the main compression regime in north-south direction to quickly significant extension in EW-direction.
【Fund】: 国家重点基础研究发展规划(编号G1999043216 G1999043211);; 中国地质调查局地质调查项目(编号K1.4—3—3);; 国土资源部专项研究计划(编号20010103)
【CateGory Index】: P618.41
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1 ZENG Qing-dong~1,LIU Jian-ming~1,CHU Shao-xiong~1,FU Guo-li~2, YU Wen-bin~3,LI Ze-ming~3,Gao Yu-you~3,LI Yuan-jiu~3, SUN Yan~1,ZHOU Ling-li~1,DUAN Xiao-xia~1,ZHANG Song~1,WANG Yong-bin~1 1.Key Laboratory of Mineral Resources/Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Chifeng Bureau of Land and Resources,Chifeng 024006,Inner Mongolia,China 3.No.243 Geological Parly of Nuclear Industry,Chifeng 024006,Inner Mongolia,China;Mesozoic Granitic Magmatism and Molybdenum Ore-Forming Processes in the Xilamulun Metallogenic Belt[A];[C];2012
2 Zhiguang Chen~(a,b),Lianchang Zhang~(a,*),Bo Wan~c,Huaying Wu~(a,b),Nathan Cleven~d ~aKey laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing,China ~bGraduate University of Chinese Academy of Sciences,P.O.Box 3908,Beijing,China ~cState Key Laboratory of Lithosphere Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing,China ~dUniversity of Waterloo,Ontario,Canada;Geochronology and geochemistry of the Wunugetushan porphyry Cu-Mo deposit in NE china,and their geological significance[A];[C];2012
3 JIANG XiaoHui~1,FAN HongRui~(1**),HU FangFang~1,YANG KuiFeng~1,LAN TingGuang~1,ZHENG XiaoLi~2 and JIN NianXian~2 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Shandong Gold Company Ltd.,Laizhou 264000,China;Comparative studies on fluid inclusion in different depths and ore genesis of the Sanshandao gold deposit,Jiaodong Peninsula[A];[C];2012
4 Huaying Wu·Lianchang Zhang·Bo Wan·Zhiguang Chen·Peng Xiang·Franco Pirajno·Andao Du·Wenjun Qu Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences, P.O.BOX 9825,Beijing 100029,People's Republic of China Graduate University of Chinese Academy of Sciences, Beijing 100049,People's Republic of China School of Earth and Environment, University of Western Australia, 35 Stirling Highway, Crawley 6005,Australia National Research Center of Geoanalysis, Beijing 100037,People's Republic of China;Re-Os and ~(40)Ar/~(39)Ar ages of the Jiguanshan porphyry Mo deposit,Xilamulun metallogenic belt,NE China,and constraints on mineralization events[A];[C];2012
5 Huaying Wu~(ab*),Lianchang Zhang~a,Bo Wan~(bc),Zhiguang Chen~(a,b),Xiaojing Zhang~a,b),Peng Xiang~(a,b) ~aKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,People's Republic of China ~bGraduate University of Chinese Academy of Sciences,Beijing 100049,People's Republic of China ~cState Key Laboratory of Lithosphere Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,People's Republic of China;Geochronological and geochemical constraints on Aolunhua porphyry Mo-Cu deposit,northeast China,and its tectonic significance[A];[C];2012
6 Qingdong Zeng,Jianming LIU,Zuolun Zhang,Weiqing Zhang,Shaoxiong Chu, Song Zhang,Zaicong Wang and Xiaoxia Duan Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,the Chinese Academy of Sciences,Beijing,China;Geology,Fluid Inclusion,and Sulfur Isotope Studies of the Chehugou Porphyry Molybdenum-Copper Deposit,Xilamulun Metallogenic Belt,NE China[A];[C];2012
7 LAN Ting-guang,FAN Hong-rui~*,HU Fang-fang,YANG Kui-feng and WANG Yong (Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Genesis of the Weishan REE deposit,Shandong Province:Evidences from Rb-Sr isochron age,LA-MC-ICPMS Nd isotopic compositions and fluid inclusions[A];[C];2012
8 XIAO Bo~(1,2),QIN Ke-zhang~1,LI Guang-ming~1,LI Jin-xiang~1,CHEN Lei~(1,2),ZHAO Jun- xing~(1,2),FAN xin~(1,2) (1 Key Lab of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029; 2 Graduate School of Chinese Academy of Sciences,Beijing 100049);Distributions and Characters of Zhibula-Langmujiaguo Skarn Cu Deposits Environing the Qulong Porphyry Cu-Mo Deposit and Their Implications for Ore-Search Towards the Deep Subsurface[A];[C];2012
9 ZHAO Jun-xing~(1,2),QIN Ke-zhang~1,LI Guang-ming,LI Jin-xiang~1) (1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029;2.Graduate School of Chinese Academy of Sciences,Beijing 100049);Characteristics of Alteration and Mineralization in the Sharang Pophyry Molybdenum Deposit in the Northern Margin of Gangdese and Conparison with Typical Porphyry Molybdenum Deposits in the World[A];[C];2012
10 Fu Zhiguo~1,Zheng Hongxing~(1,2),Weng Jichang~(1,2),Luo Mingjiu~3 (1 NO.2 Geoexploration Party of Henan Bureau of Geoexploration and Mineral Development, Xuchang,461000;2.Henan Institute of Geological Survey,Zhengzhou,450001; 3.Henan Bureau of Geoexploration and Mineral Development,Zhengzhou,450012);Physical-Chemical Mineralizational Conditions of Typical Deposits in Xiaoqinling Gold Field[A];[C];2009
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9 LUO Zhen kuan1, MIAO Lai cheng1,2, GUAN Kang1, QIU You shou1, Y. M. QIU3, N. J. McNaughton3, D. I. Groves3(1. Tianjin Geological Academy, Tianjin 300061, China; 2. Instutite of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029, China; 3;SHRIMP U-Pb zircon age of magmatic rock in Paishanlou gold mine district, Fuxin, Liaoning Province, China[J];Geochimica;2001-05
10 Qiu Ruilong; Yang Yizhong (Anhui Institute of Geological Sciences, Hefei 230001);REE CHARACTERISTICS AND GENETIC SIGNIFICANCE OF SKARN-TYPE COPPER-GOLD ORE DEPOSITS IN TONGGUANSHAN REQION[J];GEOCHIMICA;1994-04
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