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新疆彩霞山铅锌矿床地质及同位素地球化学特征
引用本文:高景刚,彭明兴,梁婷,王磊,王登红,李玉林.新疆彩霞山铅锌矿床地质及同位素地球化学特征[J].地球科学与环境学报,2007,29(2):137-140.
作者姓名:高景刚  彭明兴  梁婷  王磊  王登红  李玉林
作者单位:1. 长安大学地球科学与资源学院,陕西西安,710054
2. 新疆地质矿产勘查开发局第一地质大队,新疆昌吉831100
3. 中国地质科学院矿产资源研究所,北京100037
基金项目:中国地质调查局地质调查项目;新疆地质矿产勘查开发局资助项目
摘    要:对彩霞山铅锌矿床矿石矿物和围岩的硫、铅同位素及脉石矿物的氢、氧同位素地球化学特征进行了研究。分析结果显示,成矿物质来源于地壳和地幔的混合;硫来源主要为同化了海水硫酸盐的岩浆硫,并有少量生物还原硫参与。氢、氧同位素指示成矿流体早期可能有岩浆热液,主成矿期主要是地层中的建造水参与成矿。

关 键 词:彩霞山  矿床地质  同位素  地球化学  铅锌矿床  新疆
文章编号:1672-6561(2007)02-0137-04
修稿时间:2006-06-06

Research on Geology and Isotopic Geochemistry of Caixiashan Pb-Zn Deposit in Xinjiang
GAO Jing-gang,PENG Ming-xing,UANG Ting,WANNG Lei,WANG Deng-hong,LI Yu-lin.Research on Geology and Isotopic Geochemistry of Caixiashan Pb-Zn Deposit in Xinjiang[J].Journal of Earth Sciences and Environment,2007,29(2):137-140.
Authors:GAO Jing-gang  PENG Ming-xing  UANG Ting  WANNG Lei  WANG Deng-hong  LI Yu-lin
Abstract:The geochemical characteristic of S and Pb isotope compositions of the ore minerals and wall rocks,and H and O isotope compositions of gangue rocks from the Caixiashan Pb-Zn deposit in Xinjiang are studied.The results show that the metal is mainly derived from the mixture of mantle and crust,the magmatic sulfur,which assimilate silicon in the sea with a small amount of the sulfur made by biology in reductive condition.H and O isotopes reveal that the metallogenic fluid may has magmatic hydrothermal in early times and the formational water in the stratum participated the maineralization during the main metallizing phase.
Keywords:Caixiashan  mineral deposits  isotope  geochmistry  Pb-Zn deposit  Xinjiang
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