| 湖南黄土店金矿区变佘云煌岩的发现及其岩石化学特征 |
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| 引用本文： | 周淑芳.湖南黄土店金矿区变佘云煌岩的发现及其岩石化学特征[J].贵州工业大学学报(自然科学版),1993(1). |
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| 作者姓名： | 周淑芳 |
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| 作者单位： | 贵州工学院地质系 |
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| 摘 要： | 湖南黄土店金矿区,原被认为是粉砂岩或粘土岩分布的地方。但经笔者野外考察及室内镜下鉴定,岩石化学成份测试,岩石矿物成份的计算和图解后认为:该金矿区有云煌岩岩脉产出,并发生了浅变质作用,岩石可定名为变余云煌岩。
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| 关 键 词： | 粉砂岩 粘土岩 变余云煌岩 湖南黄土店 |
THE DISCOVERY OF BLASTOMINETTE IN THE GOLD DEPOSIT AT HUANG TU DIAN IN HUNAN AND ITS ROCK CHEMICAL FEATURES |
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| Zhou Sufang.THE DISCOVERY OF BLASTOMINETTE IN THE GOLD DEPOSIT AT HUANG TU DIAN IN HUNAN AND ITS ROCK CHEMICAL FEATURES[J].Journal of Guizhou University of Technology(Natural Science Edition),1993(1). |
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| Authors: | Zhou Sufang |
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| Abstract: | The Huang Tu Dian gold deposit in Hunan used to be thought as the distributive place for microclastic rock and clay rock. According to the inspection in the field and identification under micr- oscope in the laboratory testing of chemical composition of the rosks; and through the calculation and diagramming of the mineral composit- ion in rock,the writer believes that there are the mineral vein of blasfo-mineffe developed in this gold deposit and it had undergone a kind of metamorphism,therefore,the rock can be named as blastom- inette. |
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| Keywords: | microclastic rock clay rock blastominette Huang Tu Dian Hunan |
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