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《Mineral Deposits》 2013-02
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Re-Os dating of molybdenite from Tianbaoshan polymetallic orefield in Yanbian and its geological significance

ZHANG Yong1,SUN JingGui1,XING ShuWen2,ZHAO KeQiang1,ZHANG ZengJie2 and MA YuBo2(1 College of Earth Sciences,Jilin University,Changchun 130061,Jilin,China;2 Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China)  
The Tianbaoshan orefield,a large hydrothermal polymetallic(lead,zinc,copper,molybdenum)orefield in Yanbian,is composed of Xinxing lead-zinc deposit,Lishan lead-zinc-copper deposit and Dongfeng lead-zinc-copper-molybdenum deposit.On the basis of geological features,the authors carried out Re-Os dating,and the results show that the Re content of the molybdenite varies from 0.353×10-6 to 9.306×10-6,the model ages range from 174.7 to 200.3 Ma with the weighted mean age being(194.6±3.9)Ma and the isochron age bring(196.6± 2.5)Ma(MSWD=0.94,n=9).These data indicate that molybdenum mineralization took place in early Jurassic,and the geodynamic setting was closely related to the extension from the continental collision between the North China Plate and the Siberia Plate.The ore-forming materials might have been derived mainly from the crust.Combined with the high precision chronologic data of regional intrusions,the authors have arrived at the conclusion that Mo mineralization of the middle and east part of Jilin Province can be divided into 2 epochs:Early Jurassic(196.6~186 Ma)and Middle Jurassic(176.9~166.9 Ma),with the Middle Jurassic epoch having stronger mineralization.
【Fund】: 中国地质调查计划项目(资〔2010〕矿评01-26-06);; 吉林省科技发展规划项目(批准号:20100450);; 国家自然科学基金项目(批准号:41172072)的联合资助
【CateGory Index】: P618.65;P597.3
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