| 庐山温泉的形成条件及成因研究 |
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| 引用本文： | 李学礼 史维浚. 庐山温泉的形成条件及成因研究[J]. 华东地质学院学报, 1992, 15(3): 229-233 |
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| 作者姓名： | 李学礼 史维浚 |
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| 作者单位： | 华东地质学院水文地质系，华东地质学院水文地质系，华东地质学院水文地质系，华东地质学院水文地质系 林冶金地质学院水工系主任 |
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| 摘 要： |
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| 关 键 词： | 庐山 温泉 同位素 成因 |
THE FORMATION CONDITION OF THE LUSHAN HOT SPRING AND ITS GENESIS |
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| Li Xueli Shi Weijun Yang Zhongyao. THE FORMATION CONDITION OF THE LUSHAN HOT SPRING AND ITS GENESIS[J]. Journal of East China Institute of Technology, 1992, 15(3): 229-233 |
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| Authors: | Li Xueli Shi Weijun Yang Zhongyao |
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| Affiliation: | Department of Hydrogeology |
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| Abstract: | The Lushan Hot Spring is controlled by a recent active deep fault. According to the tectonic condition and hydrochemical compositions, it is similar to the pyrenees mineral water in Europe. The data of the oxygen and hydrogen isotopes show that the source of the Lushan hot spring is derived from meteoric water. Its supply zone is the Lushan ancient razed basin located at altitude about 1000m, the circulation depth of ground-water should be less than 3700m, the age of the hot spring is older than 30 years. |
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| Keywords: | Lushan Thermal springs isotope cause of formation |
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