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Geochemical Characteristics of Xiaogouli-Sanyangba Gold Deposit of Xihe-Chengxian Basin in Gansu Province
详细信息   
摘要

On the basis of detailed investigation of geological setting and ore deposit features, this paper deals with geochemistry and sulfur and lead isotopes of Xiaogouli-Sanyangba gold deposit in Xihe-Chengxian basin, Gansu Province. The results show that the Co/Ni of pyrite is mostly more than 1 indicating that the ore-forming material is derived from magmatic-hydrothermal fluid. Analysis showed that in liquid pahse Na+, K+ are the dominant cation and Cl- the dominant anion, in gas phase H2O and CO2 dominant. The homogenization temperature, salinity range in 115 to 205 and 7.2% to 11.5%, respectively. The ore fluid is mainly composed of meteoric water.

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