| 豫西祁雨沟金矿床成矿流体岩浆来源的流体包裹体和稳定同位素证据 |
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| 引用本文： | 范宏瑞,胡芳芳,杨奎锋,金成伟.豫西祁雨沟金矿床成矿流体岩浆来源的流体包裹体和稳定同位素证据[J].矿物学报,2009,29(Z1). |
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| 作者姓名： | 范宏瑞 胡芳芳 杨奎锋 金成伟 |
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| 作者单位： | 中国科学院,地质与地球物理研究所,北京100029 |
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| 摘 要： | Gold ores of the Qiyugou deposit in the eastern part of the Xiong' ershan region are hosted in breccia pipes within a Mesozoic granitic porphyry. Three stages of alteration-hydrothermal activity are recognized within the Qiyugou breccias. The first stage of hydrothermal metasomatism produced extensive Kfeldspar alteration, The second stage is associated with deposition of gold and base metal sulfide minerals.
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