| 吉林省荒沟山金矿床地质特征及成因 |
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| 引用本文： | 郑传久.吉林省荒沟山金矿床地质特征及成因[J].吉林地质,1995,14(3):1-16. |
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| 作者姓名： | 郑传久 |
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| 作者单位： | 吉林省地质科学研究所 |
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| 摘 要： | 荒沟山金矿床明显受构造控制，矿体多呈复杂的脉体充填于大理岩开放空间中，成矿为多期次、热液角砾岩化多期次的特点，成矿流体以大气水为主，具有浅成、低温、低盐度和近中性的成矿环境，属于浅成低温热液成因金矿床。
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| 关 键 词： | 矿床特征 地球化学 成矿作用 金矿床 成因 |
THE GEOLOGICAL FEATURES AND ITS ORIGIN OF THE HUANGGOUSHAN GOLD DEPOSIT,JILIN PROVINCE |
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| Zheng Chuanjiu.THE GEOLOGICAL FEATURES AND ITS ORIGIN OF THE HUANGGOUSHAN GOLD DEPOSIT,JILIN PROVINCE[J].Jilin Geology,1995,14(3):1-16. |
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| Authors: | Zheng Chuanjiu |
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| Abstract: | It is quite obvious that the Huanggoushan gold deposit is controlled by the structures,and the ore bodies as the complicated veins are mostly filled in the open-spaces of marble,showing the metallogenic characteristics of multiple stages with multiple hydrothermal brec-ciation. The ore-forming fluid is mainly meteorological water,having epithermal,low salini-ty near intermediate mineralizing setting and belonging to epithermal hydrothermal deposit. |
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| Keywords: | Characteristics of ore deposit Geochemistry Ore-forming process Ori-gin of ore deposit The Huanggoushan gold deposit |
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