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《Geotectonica Et Metallogenia》 2004-02
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STUDY ON FLUID INCLUSIONS OF TUANJIEGOU GOLD DEPOSIT IN HEILONGJIANG PROVINCE AND IMPLICATIONS FOR ITS GENESIS

WANG Keyong, REN Yunsheng, CHENG Xinmin and DAI Junzhi (College of Earth Sciences, Jilin University, Changchun, JL 130061,China)  
A systematic study on fluid inclusions developed in quartz phenocryst of ore-bearing porphyry as well as in chalcedony quartz in ores of Tuanjiegou gold deposit was carried out, the results show that daughter crystal-bearing three-phase, aqueous two-phase and pure aqueous phase etc. occur in the fluid inclusions of quartz phenocrysts from ore-bearing porphyry, while aqueous two-phase primary fluid inclusions dominate in chalcedony quartz from the ores. Microthermometric study testifies that the temperature of ore-forming solutions is between 130 and 370℃, whereas salinity varies from 2-10wt%NaCl. These values are coincident with those for aqueous two-phase fluid inclusion in quartz phenocryst. Based on the compositional analytical results of fluid inclusions, it is concluded that the ore-forming fluids mainly originated from magmatic evolution and meteoric water. The deposit is of epithermal origin related to the intrusive activities of porphyry.
【Fund】: 吉林大学青年教师基金;; 国土资源部矿产资源定量勘查与评价开放研究实验室基金联合资助
【CateGory Index】: P618.51
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