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The Sources of OreForming Fluid in the Huize LeadZinc Ore Deposits：Evidences for WaterRock Reaction

ZHANG Zhen-liang1,2,HUANG Zhi-long1,RAO Bing3,GUAN Tao1,2,YAN Zai-fei1,2   

  1. 1. Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry，Chinese Academy of Sciences,Guiyang 550002, China;2. Postgraduate School of the Chinese Academy of Sciences, Beijing 100039,China;3. Department of Earth Sciences, State Key Laboratory of Mineral Deposit Research, Nanjing University，Nanjing 210093,China
  • Received:2004-11-02 Revised:1900-01-01 Online:2005-09-26 Published:2005-09-26
  • Contact: ZHANG Zhen-liang

Abstract: The characters of fluid inclusions in calcite and waterrock reaction of the ore deposits was systematical studied. It is suggested that the ore deposit under study was relative to the mixing of the lowtemperature and hightemperature hydrothermal solutions. δ18O and δD values of oreforming fluid of different ore bodies are unanimous, thus indicating that fluid homogenisation once happened before the formation of oreforming fluid. The oreforming fluid in fluid reservoir is of multiple derivation of the mixed circular waters in the strata, metamorphic fluids and magmatic waters.

Key words: oreforming fluid, fluid inclusion, H and O isotopes, fluid fixing, Huize leadzinc ore deposits

CLC Number: 

  • P618.4
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