| 豫西公峪金矿床特征及成矿机制探讨 |
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| 引用本文： | 张侍威.豫西公峪金矿床特征及成矿机制探讨[J].地质与勘探,2004,40(5):12-15. |
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| 作者姓名： | 张侍威 |
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| 作者单位： | 河南省有色金属地质矿产局,郑州,450052 |
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| 摘 要： | 文章介绍了公峪构造蚀变岩型金矿床地质地球化学特征,依据稳定同位素资料,推断该矿床成矿流体来自于深源及大气降水,流体的混合作用导致了公峪金矿床矿石矿物的沉淀.
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| 关 键 词： | 地质特征 成矿流体 硫氢氧同位素 金矿床 公峪 |
| 文章编号： | 0495-5331(2004)05-0012-04 |
| 修稿时间： | 2004年3月12日 |
GEOLOGICAL FEATURES AND ORE-FORMING MECHANISM OF ALTERED TECTONITE-TYPE GONGYU GOLD DEPOSIT,WESTERN HENAN PROVINCE |
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| ZHANG Shi-wei.GEOLOGICAL FEATURES AND ORE-FORMING MECHANISM OF ALTERED TECTONITE-TYPE GONGYU GOLD DEPOSIT,WESTERN HENAN PROVINCE[J].Geology and Prospecting,2004,40(5):12-15. |
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| Authors: | ZHANG Shi-wei |
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| Abstract: | Geological and geochemical characteristics of the Gongyu gold deposit was introduced. Based on stable isotope data, it is concluded that the ore-forming fluids are derived from the deep-source fluid and the meteoric water. fluid Mixing resulted in the ore deposition in the Gongyu gold deposit. |
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| Keywords: | geological characteristics ore-forming fluid stable isotope Gongyu gold deposit |
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