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矿床地质  2005 

西藏冈底斯斑岩铜矿带厅宫铜矿床流体包裹体研究

Keywords: 地球化学,流体包裹体,出溶,斑岩铜矿,厅宫,冈底斯,西藏

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Abstract:

厅宫斑岩铜矿床是西藏冈底斯斑岩铜矿带上重要的矿床之一。为了探明该矿床成矿流体的成分及温压条件等物理化学性质,文章对厅宫铜矿各蚀变阶段石英脉及石英斑晶中的流体包裹体进行了显微测温、四极杆质谱、离子色谱和激光拉曼探针分析,结果表明:厅宫铜矿成矿流体为高温、高盐度岩浆热液,成矿事件主要发生在340~380℃,成矿过程中流体发生了沸腾;成矿流体中气相成分以H2O为主,还含有一定量的CO2及少量的CH4、H2S、C2H6等气体;液相中离子以K+、Na+、Cl-、SO2-4、F-等为主,还含有少量的Ca2+、Mg2+等;另外,出现大量气泡先消失、子矿物后熔融的Ⅲa类包裹体,表明有些成矿流体可能直接来源于深部岩浆的出溶作用。

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