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《Geotectonica Et Metallogenia》 2004-04
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DISCUSSION ON THE METALLOGENIC DEPTH OF SKARN TYPE GOLD DEPOSITS IN TONGLING AREA, ANHUI PROVINCE

REN Yunsheng~1, LIU Liandeng~1, WAN Xiangzong~2 and LIU Lianggen~3 (1. College of Earth Sciences, Jilin University, Changchun, JL 130061, China; 2. Baocun Gold Mine in Shizishan District, Tongling, Anhui 244031, China; 3. No. 321 Geological Team, Tongling, Anhui 244033, China)  
The metallogenic depth of the Baocun and Chaoshan skarn type gold deposits are estimated in this paper based on both fluid inclusions and geological features. Features of the intrusions associated with gold mineralization and the vertical lengths of the gold ore bodies, mineral compositions of the gold ores as well as shapes of the gold minerals in the two mines indicate that the gold mineralization in the two deposits took place in shallow or middle to shallow depths. Homogenization temperature of the fluid inclusions from quartz and calcite formed at various stages are determined. The metallogenic pressure estimated by fluid inclusions is 650×10~5~850×10~5 Pa, equivalent to depth from 2.5 to 3.2 km. Metallogenic depth estimated by fluid inclusions is similar to that estimated by geological features of the deposits. The conclusion can be drawn that skarn type gold deposits in Tongling area were formed at middle to shallow depth. The phase separation and boiling of fluids played an important role in the gold mineralization.
【Fund】: 吉林大学青年教师基金项目资助.
【CateGory Index】: P618.51
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