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《Gold Science and Technology》 2009-05
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Molybdenite Re-Os Age and Other Geological Meaning of Machangqing Porphyry Copper,Molybdenum Deposit

XING Junbing1,2,GUO Xiaodong1,2,QU Wenjun4,WANG Zhihua2,LI Hanguang31.China University of Geoscience,Beijing 100083,China;2.Gold Geological Institute of CAPF,Langfang 065000,Hebei,China;3.No.3 General Gold Party of CAPF,Chengdu 610036,Sichuan,China;4.National Geological Experiment and Test Center,Beijing 100037,China  
Machangqing alkalite intrusive rock is multiperiodic and multistage magmatic activity superimposed intrusive composite rock in west of Yunnan.The time limit of magmatic activity is 52~29 Ma,the earliest time began at 52 Ma,mid time of it is 47~42 Ma,and the latter time of it is 37~29 Ma.Using ICP-MS testing the age of molybdenite Re-Os isotope of Baoxingchang porphyry copper,molybdenum deposit,get the pattern age is 34.9±0.8~36.0±0.5 Ma,the average of it is 35.3±0.7 Ma,which indicated that metallogenic time limit is about 35~36 Ma.The result of above tallied with later granite-porphyry(29~37 Ma) of Machangqing complex rock,showed that mineralization mainly related with later magmatic invasive activity.The existing two ore occurrence shape and mineral compound form of Machangqing copper,molybdenum poly metallic ore deposit belonged to the production of syn-mineralization;the different representation in different space of syn-mineralization,belonged to same mineralization system.Porphyry copper,molybdenum deposit of Jinshajiang-Ailaoshan mineralization belt was the production of the syn-mineralization,and mineralization time limit focused in 35~36 Ma.
【Fund】: “十一五”国家攻关项目(编号:2006BAB01B10);; 武警黄金指挥部专项基金(编号:HJ07-02)联合资助
【CateGory Index】: P578.291
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