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《Acta Geoscientica Sinica》 2012-04
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S,Pb Isotope Characteristics of the Ga'erqiong Gold-Copper Deposit in Tibet:Tracing the Source of Ore-forming Materials

YAO Xiao-feng 1),TANG Ju-xing 2,3),LI Zhi-jun 3),DENG Shi-lin 4),HU Zheng-hua 3),ZHANG Zhi 3) 1) China University of Geosciences,Beijing 100083;2) MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037;3) Chengdu University of Technology,Chengdu,Sichuan 610059;4) Geophysical Prospecting Party of Sichuan Bureau of Geology and Mineral Resources,Chengdu,Sichuan 610000  
The Ga'erqiong copper-gold deposit,a skarn-type and breccia-type copper-gold(iron) deposit related to porphyry,was discovered in recent years in the western Bangong Co-Nujang metallogenic zone,Tibet.Based on the study of the S and Pb isotope characteristics of pyrite and chalcopyrite within the skarn ore,the authors traced the source of ore-forming materials,and indicated regional ore-forming metallogenic regularity based on a comparison with the characteristics of regional mineral resources.It is shown that the δ 34 S value of the minerals is in the range of-2.9‰~0.5‰ with an average of-1.1‰,and the δ 34 S histogram is distributed approximately in a tower shape,which indicates a mantle source.The 208 Pb/204 Pb value is between 38.384 and 39.134,and the 207 Pb/204 Pb value is between 15.577 and 15.725,and the 206 Pb/204 Pb value is between 18.112 and 18.615,and the μ value is between 9.44 and 9.69,which indicate that Pb was derived from a orogenic belt source composed of the upper crust and the mantle.It is inferred that the ore-forming materials of the Ga'erqiong deposit was mainly from materials with mantle characteristics and Nyainqentanglha basement gneiss.During the arc-landmass collision between southern Qiangtang-Sanjiang composite plate and Gandise-Nyainqentanglha plate in late Cretaceous,a Cu-Au porphyry-skarn metallogenic series related to magma which was derived from the upper mantle or the juvenile crust and contaminated by the upper crust materials formed in the Coqen-Xainza volcanic-magmatic arc at the south edge of western Bangong Co-Nujang suture zone.
【Fund】: 公益性行业科研专项项目(编号:201011013-3);; 国家973项目(编号:2011CB403103);; 西藏卓朗基矿业投资有限公司详查项目联合资助
【CateGory Index】: P618.41;P597
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