南京大学学报(自然科学版) ›› 2012, Vol. 48 ›› Issue (3): 266277.
徐九华**,张国瑞,魏浩,林龙华,吴晓贵
Xu Jiu一hua,Zhang Guo一Rui,Wei Hao ,Lin Long一Hua ,Wu Xiao一Gui
摘要: 流体包裹体的捕获压力研究是成矿压力和成矿深度估算的常用方法,其结果受多种因素的影响.在综合考虑脉状金矿的地质特征、所研究包裹体体系的基础上,研究了脉状金矿床富金石英脉的成矿压力.该类金矿床富金阶段的最低形成压力范围较宽,从小秦岭烟灰色含金石英脉阶段的270-290MPa、乌拉山含明金石英脉的250 MPa,到东坪富金石英脉的70 - 160 MPa.流体富CO2是脉状金矿一个重要特征,尤其是造山型金矿及与侵入岩有关的金矿,估算其流体捕获压力时应该利用CO2一H2O体系或CO2 - H2O-NaCI体系的压力计方法.压力与CO2部分均一温度(Tm,co2)有明显的负相关关系,反映了CO2密度与压力的密切关系.CO2丰度高且密度较高的金矿床具有较高的成矿压力.为使获得的数据具有可比性,脉状金矿的成矿压力及深度估算应考虑包裹体类型、寄主矿物所处的构造环境、
断裂性质、断裂/矿脉的产状、岩石类型及密度等主要因素.
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