ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西藏邦铺铅锌矿床S、Pb、C、O同位素组成及成矿物质来源研究
  
关键词:sulfur isotope  lead isotope  carbon and oxygen isotope  source of ore-forming materials  crustal contamination  ore-forming fluid  Bangpu
基金项目:国家973项目(编号: 2011CB403103);国土资源地质大调查项目(编号: 1212010012005)
作者单位
王立强 中国地质科学院矿产资源研究所 
罗茂澄 中国地质大学(北京)地球科学与资源学院 
袁志洁 中国地质科学院 
陈伟 成都理工大学地球科学学院 
冷秋锋 成都理工大学地球科学学院 
张学全 西藏地勘局地热地质大队 
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摘要:
Sulfur, Lead, Carbon and Oxygen Isotope Composition and Source of Ore-forming Materials of the Bangpu Pb-Zn Ore Deposit in Tibet
      The Bangpu Pb-Zn deposit, formed in the periphery of the porphyry mineralization body of the ore district, is a skarn deposit with relatively rich ore grade, and the ore-forming elements are dominated by lead and zinc, without copper basically. Main metal sulfides were objects of this study, and S and Pb isotopic methods were used to investigate the source of the ore-forming minerals. The results show that the δ34S values of the ore metal sulfides have a wide distribution, and mainly vary in the range of –3.7‰– –0.7‰, with the characteristics of tower distribution, and that these sulfur materials were mainly derived from the magma. Lead isotopes of the ore have stable composition and are positive common lead. The high μ values (larger than 9.58) of ore lead and the distribution characteristics of the data points in the evolution diagram of tectonic environment indicate that the ore lead was mainly derived from the upper crust. A comparison between this deposit and the nearby Zhibula and Jiama deposits shows that sulfur of these three deposits was exclusively derived from magma, and their metal materials show a certain regular pattern in source space, i.e., the contamination of crustal source material increased from south to north in the Qulong-Jiama-Bangpu ore district. Carbon and Oxygen isotope compositions of marble and calcite show that carbon in ore-forming fluid was mainly derived from the magma whereas the carbonate formation provided parts of other ore-forming materials.
WANG Li-qiang,LUO Mao-cheng,YUAN Zhi-jie,CHEN Wei,LENG Qiu-feng,ZHANG Xue-quan.2012.Sulfur, Lead, Carbon and Oxygen Isotope Composition and Source of Ore-forming Materials of the Bangpu Pb-Zn Ore Deposit in Tibet[J].Acta Geoscientica Sinica,33(4):435-443.
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