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《Geochimica》 1998-02
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FLUID MIGRATION-REACTION MODEL OF ZIJINSHAN DEPOSIT AS TRACED BY VARIATION OF OXYGEN ISOTOPE COMPOSITIONS

Hua Renmin;Hu Jinhua;Huang Yaosheng;Li Zhenmin (State Key Laboratory of Research for Mineral Deposits, Nanjing University, Nanjing 210093)  
Based on the variation of oxygen isotope compositions of altered rocks from different sites and depths in Zijinshan epithermal An-Cu deposit as well as data from hydrogen and oxygen isotope compositions of ore solution and fluid inclusion studies,the present paper discusses the source and migration-reaction mechanism of the ore-forming fluid. It is concluded that Zjinshan deposit formed mainly by the convective circulation of meteoric water. During the recharge and discharge processes of meteoric water, water-rock reaction and associated isotOPe exchange took place under different temperature and W / R conditions, resulting in the spaital variation of oxygen isotope compositions of altered rocks. An inversion calculation of δ13O values of altered rocks is conducted, which is in good accordance with measured values, also proving the fluid migration-reaction model of meteoric water in the ore formation.
【Fund】: 国家自然科学基金!49372108
【CateGory Index】: P611
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