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地球学报  2009 

冷水坑斑岩型银铅锌矿床成矿流体特征研究

DOI: 10.3975/cagsb.2009.05.07

Keywords: 斑岩型矿床,成矿流体,地球化学

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Abstract:

斑岩型银铅锌矿床世界上并不多见,目前我国典型斑岩型银铅锌矿床仅冷水坑一处。笔者通过对冷水坑斑岩型银铅锌矿床的流体包裹体地球化学、稳定同位素地球化学研究,结合岩相学研究、激光拉曼探针(LRM)和扫描电镜/能谱(SEM/EDS)测试,揭示了冷水坑斑岩型银铅锌矿床成矿流体特征及演化过程,并进一步探讨了成矿物质来源和矿床成矿机制。研究表明,冷水坑矿床成矿流体及主要成矿元素(硫)来自于斑岩系统,大气水在整个成矿过程中均有不同程度的参与。

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