湖南黄沙坪铅锌多金属矿床铅、硫同位素地球化学特征 |
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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) |
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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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