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《GEOCHIMICA》 1995-S1
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STUDY ON FLUID INCLUSIONS AND HYDROGEN AND OXYGEN ISOTOPE GEOCHEMISTRY OF RUSHAN GOLD DEPOSIT IN SHANDONG PROVINCE

Zhai Jianping; Hu Kai; Lu Jianjun (Department of Earth Sciences, Nanjing University, Nanjing 210008)  
The Rushan gold deposit, one of the important quartz-vein type gold deposits,is located in the Kunyushan granitic pluton. It lies in the central part of the Muping-Rushan gold metallogenic belt. A detailed study on fluid inclusion geochemistry indicates that the gaseous phase of the fluid inclusions is dominated by H_2O and CO_2, while the liquid phase is poor in Na+, K+, and rich in Ca(2+), Mg ̄(2+), and characterized by Na ̄+/K ̄+1 and Ca ̄(2+)+Mg ̄(2+)Na ̄++K ̄+. The salinity (wt.% NaCl equiv.) of the mineralizing liquid ranges from 5 to 9, the main mineralization stage has a temperature of about 220-280℃, and the late stage temperature is at about 130-200℃. The isotopic ages of the Kunyushan pluton and Rushan gold deposit are 134.3-124.5Ma and 80±Ma, respectively, indicating a great time interval between the crystallization of the pluton and the formation of the deposit (45-55Ma). The hydrogen and oxygen isotopic data show that the mineralizing solution is mainly derived from meteoric water. A genetic model is proposed to explain the metallogenetic mechanism of the gold deposit.
【Fund】: 国家自然科学青年基金
【CateGory Index】: P618.5
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