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《Southern Metals》 2011-03
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Characters of the inclusions in Zhijiadi Ag-Pb-Zn deposit,and the origin of their hydrothermal solution

HE Yu-ming,YANG Mu(School of Geologic Science and Environmental Engineering,Central-South University,Changsha 410083,Hunan)  
The Ag-Pb-Zn deposit in Zhijiadi,Shanxi province,a large Yanshanian stage volcanic rock-related deposit,is located on the North margin of Huabei Plate.Most fluid inclusions are secondary bead-like,or pseudo-secondary ones.Three types of fluid inclusions,namely gas-liquid inclusion(Ⅰ),liquid-gas inclusion(Ⅱ),and liquid inclusion(Ⅲ),can be discriminated with microscope.Type Ⅰ inclusions have homogenization temperatures of 142~170 ℃ and liquid/gas ratios of 15~25%;type Ⅱ inclusions have homogenization temperatures of 160~235 ℃ and liquid gas/ratios of more than 80%;and type Ⅲ inclusions have homogenization temperatures of 120~140 ℃ and liquid gas/ratios of 0%.With a salinity of 0.2~1.8% and homogenization temperatures of 120~235 ℃,the fluid inclusions show a falling tendency of the salinity-homogenization temperature,and hence a dilution process of the ore-bearing hydrothermal solution.Moreover,lots of other traits of Zhijiadi inclusions demonstrate that the ore-bearing hydrothermal solution has even been mixed with meteoric water.These traits contained a Na+/k+ ratio ≥1,a pH≥ 7,a δ18OH2O= 5.47,and a δD =-83,as well as complex gas components.
【CateGory Index】: P618.2
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