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Discovery of chalcopyrite daughter mineral in polyphase fluid inclusions from Yanyuan porphyry copper deposit, Sichuan Province

机译:四川盐源斑岩铜矿床多相流体包裹体中黄铜矿子矿的发现

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摘要

The study on polyphase fluid inclusions of porphyry copper deposits has always attracted much attention of geologists. In the early 1980s, the chalcopyrite daughter mineral in the fluid inclusions was recorded by a scanning electron microscope in theporphyry copper deposits of West America. However, such a study was poorly reported. In recent years we have studied the Yanyuan porphyry copper deposit in geology and geochemistry. Further study of fluid inclusions with electron microprobe shows the common existence of chalcopyrite daughter mineral in addition to halite in fluid inclusions, suggesting an ore-forming fluid highly enriched in ore-materials such as Cu.
机译:斑岩型铜矿床多相流体包裹体的研究一直引起地质学家的广泛关注。在1980年代初期,通过扫描电子显微镜在西美洲斑岩铜矿床中记录了流体包裹体中的黄铜矿子矿。但是,这样的研究报道很少。近年来,我们在地质和地球化学方面研究了盐源斑岩铜矿床。用电子微探针对流体包裹体的进一步研究表明,除了流体包裹体中的岩盐之外,黄铜矿子矿物也普遍存在,这表明成矿流体高度富集了诸如铜等矿石物质。

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