摘要: 河南省新县宝安寨钥矿床位于大别造山带西部,属于斑岩型钥矿床.木文对主成矿期矿化石英脉进行了流体包裹体岩相学观察和显微测温.研究表明,捕获的流体包裹体可分为富液相两相水溶液包裹体、富气相两相水溶液包裹体和含子矿物三相水溶液三类包裹体.包裹体均一温度的峰值为220?C一240?C,盐度峰值分别为2%-4%(NaCleq)低盐度区间和46%-48%(NaCleq)含子晶的高盐度区间,密度为0. 58 g/cm3-1. 05 g/cm3.激光拉曼光谱分析表明,流体包裹体的组分简单,以水蒸汽为主,含有少量的CO2.包裹体具有典型的氧同位素漂移特征,指示岩浆热液和大气降水混合作用.因此,我们认为宝安寨钥矿床属中一高温浅成热液矿床,流体混合作用可能是矿床形成的主要机制.
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