ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
湖南黄沙坪铅锌多金属矿床铅、硫同位素地球化学特征
  
关键词:Pb  S isotopes  Huangshaping lead-zinc deposit  ore
基金项目:国家自然科学基金项目(编号:2004BA615-02)
作者单位E-mail
息朝庄 中南大学 地学与环境工程学院湖南长沙 410083 xczcsummmmmm@126.com 
戴塔根 中南大学 地学与环境工程学院湖南长沙 410083  
刘悟辉 中南大学 地学与环境工程学院湖南长沙 410083  
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摘要:
Lead and Sulfur Isotope Geochemistry of the Huangshaping Lead-Zinc Deposit, Hunan Province
      The Huangshaping lead-zinc deposit is one of the typical deposits in Xiangnan (southern Hunan Province). This deposit occurs mainly in granite-porphyry and quartz porphyry. The ores are mainly composed of Pb, Zn sulfides in SN-trending Baoling reversed anticline and Guanyindazuo reversed anticline. Sulfur isotope analyses show that δ34S values of pyrites vary in the range of -2.2‰~17.2‰. Pb isotope analyses reveal that 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios of the ore lead are 17.893~18.772, 15.580~16.045 and 38.490~41.560 respectively. The research results suggest that sulfur might have been derived from the mixing effect of magma and seawater(strata). The research also shows that anomalous lead has derived from magma
XI Chao-zhuang,DAI Ta-gen,LIU Wu-hui.2009.Lead and Sulfur Isotope Geochemistry of the Huangshaping Lead-Zinc Deposit, Hunan Province[J].Acta Geoscientica Sinica,30(1):89-94.
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