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| 江西永丰南坑萤石矿床地质特征控矿地质条件及成因 | |
| 引用本文： | 文化川,侯光仪. 江西永丰南坑萤石矿床地质特征控矿地质条件及成因[J]. 西南科技大学学报, 1993, 0(4) |
| 作者姓名： | 文化川 侯光仪 |
| 作者单位： | 四川建材学院资源工程系(文化川)，四川建材学院资源工程系(侯光仪) |
| 摘 要： | 根据产于花岗岩断裂破碎带中的脉状萤石矿床地质特征,控矿地质条件及地下水热液成矿作用研究,表明产于花岗岩断裂破碎带中的脉状萤石矿床并不属于岩浆期后热液矿床。 |
| 关 键 词： | 花岗岩 萤石矿床特征 控矿条件 成因 |
The Geological Charecteristics Controlled Geological Conditions and Geneses of Nankeng Fluorite Depasit in Yongfeng Jiangxi Province |
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| Wen Huachuan Hou Guangyi. The Geological Charecteristics Controlled Geological Conditions and Geneses of Nankeng Fluorite Depasit in Yongfeng Jiangxi Province[J]. Journal of Southwest University of Science and Technology, 1993, 0(4) | |
| Authors: | Wen Huachuan Hou Guangyi |
| Affiliation: | Southersy Institute of Technology |
| Abstract: | According to the geological characteristies of Nankeng vein fluorite deposit located in fractured zone of granite, the confrolled geological conditions and groundwater hydro -thermal mineralizafion are discussed in this paper. The study show that the mineralizafian of vein fluorite deposit located in tractured zone of granite is not belong to post - magmafic hyrotherinal deposit. |
| Keywords: | granife fluorite deposit characteristis geneses |
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