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热液金矿床控矿断裂性质与成矿流体的物理化学

Tectonic Environment of Hydrothermal Gold Deposits and Physico_chemistry of Ore_forming Fluid

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【作者】 徐九华谢玉玲申世亮

【Author】 Xu Jiuhua Xie Yuling Shen Shiliang (Department of Geology,University of Science and Technology Beijing)

【机构】 北京科技大学资源工程学院

【摘要】 热液金矿床的成矿物理化学条件与控矿断裂构造环境有着密切联系。作者对比了不同构造环境(小秦岭、焦家、玲珑和太白金矿)流体包裹体物理化学参数特征,表明韧性剪切带环境中的金矿成矿流体压力大、CO2/H2O数值也高。不同构造环境中流体K+/Na+、F-/Cl-的差别不仅与容矿岩石化学特征有关,也与构造应力作用有关,同一矿田内,甚至同一断裂带内,因所处构造部位不同,成矿流体压力也不同,致使其他物理化学参数的系统变化,这对地质找矿具有实际意义。

【Abstract】 Metallogenic physico_chemical conditions of hydrothermal gold deposits are greatly associated with ore_controlling fault environment .A comparison of physico_chemical parameters of fluid inclusions from different tectonic environments(including Xiaoqinling,Jiaojia,Linglong and Taibei gold deposits)has been studied .The result shows that the pressures of ore_forming fluids of gold deposits in ductile shear zones are higher,so the values of CO 2/H 2O of fluid inclusions are high.K +/Na + and F -/Cl - of fluid inclusions varies in different tectonic environments,which is not only related to chemistry of host rocks,but also related to tectonic stress.Because ore_forming fluid pressures vary,other parameters of physico_chemistry change sysmaticly,very useful for gold prospecting

【基金】 冶金工业部人教司有偿与资助基金
  • 【分类号】P618.510.2
  • 【被引频次】16
  • 【下载频次】255
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