| 浏阳市连云山矿泉水特征及形成机制 |
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| 引用本文： | 杨顺泉,李佐海.浏阳市连云山矿泉水特征及形成机制[J].湖南地质,1998,17(3):169-173,177. |
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| 作者姓名： | 杨顺泉 李佐海 |
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| 作者单位： | 湖南省地质矿产厅 |
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| 摘 要： | 连云山矿泉水是一处优质偏硅酸饮用天然矿泉水，其形成受深大断裂控制，有良好的成矿条件和资源潜力。长－柏大断裂带为一个矿泉水出露带，矿泉水资源远景巨大。
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| 关 键 词： | 矿泉水 成矿条件 连云山 形成机制 |
CHARACTERISTICS AND FORMING MECHANISM OF LIANYUNSHAN MINERAL SPRING WATER IN LIUYANG CITY |
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| Yang Shunquang Li ZuohaiHunan Bureau of Geology and Mineral Resources,Changsha.CHARACTERISTICS AND FORMING MECHANISM OF LIANYUNSHAN MINERAL SPRING WATER IN LIUYANG CITY[J].Hunan Geology,1998,17(3):169-173,177. |
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| Authors: | Yang Shunquang Li ZuohaiHunan Bureau of Geology and Mineral Resources Changsha |
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| Institution: | Yang Shunquang Li ZuohaiHunan Bureau of Geology and Mineral Resources,Changsha 410011 |
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| Abstract: | Lianyunshan mineral spring mineral spring water is the good quality metasilicate drinking nature water.Its forming is controlled by the deep and great fault,and has the good metallogenic conditions and resources potentiality.Changshujie-Bojiashan fault zone is the mineral spring water exposure belt,and there is the great resources prospect. |
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| Keywords: | Mineral spring water Metallogenic condition Lianyunshan Liuyang |
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