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Studies on the fluid inclusions from Lishan gold deposit in Jiapigou, Jilin Province, China

机译:吉林省贾pi沟Li山金矿床流体包裹体研究

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Lishan gold deposit is a large-scale quartz vein type gold deposit in Jiapigou region.Fluid inclusions in quartz vein type ores taken from No.5 ore vein explain that there are 3 types of primary fluid inclusions i.e. Ⅰ Carbon dioxide, ⅡCarbon dioxide-bearing three-phase, Ⅲ aqueous phase etc. The microthermometric study of fluid inclusions showed that the homogenization temperature of every kind of fluid inclusions ranges from 218.2°C to 420°C; Salinity ranges from 3.1wt%NaCl equiv, to 11.4 wt%NaCl equiv. The intergrowth of type Ⅰ, Ⅱ and Ⅲ fluid inclusion,combined with analysis of composition of Carbon dioxide phase of fluid inclusions reflect that it is immiscible NaCl-H2O-CO2 system. According to the temperature-pressure estimation method in immiscible systems, we calculated the metallogenic temperature is 335-415 °C and metallogenic pressure is 750-1250×105 Pa, indicating to formed in a depth of 4.4-7.5 km.
机译:Jia山金矿床是嘉pi沟地区的大型石英脉型金矿床。从5号矿脉提取的石英脉型矿石中的流体包裹体说明,主要的流体包裹体类型为Ⅰ,二氧化碳,Ⅱ,含二氧化碳。流体夹杂物的微热学研究表明,每种流体夹杂物的均质温度范围为218.2°C至420°C。盐度范围从当量的3.1wt%NaCl到当量的11.4wt%NaCl。 Ⅰ,Ⅱ,Ⅲ型流体包裹体的共生性,结合流体包裹体二氧化碳相的组成分析表明,该体系与NaCl-H2O-CO2体系不混溶。根据不混溶系统中的温度-压力估算方法,我们计算出成矿温度为335-415°C,成矿压力为750-1250×105 Pa,表明形成于4.4-7.5 km的深度。

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