| 四川峨眉山荷5井地热水特征及其成因分析 |
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| 引用本文： | 齐春梅,线恒林.四川峨眉山荷5井地热水特征及其成因分析[J].成都理工大学学报(自然科学版),2000,27(3):308-311. |
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| 作者姓名： | 齐春梅 线恒林 |
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| 作者单位： | 西南石油局第二地质大队,四川自贡 643013 |
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| 摘 要： | 通过对四川峨眉山荷5井地质、水文地质、水化学特征分析研究,认为地热水是在构造复杂、新构造运动剧烈区,大气降水下渗经深部循环和溶滤作用并与少量沉积水混合而成,为受断裂控制的深循环型中、低温地下热水.
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| 关 键 词： | 喀斯特地下水 淋滤作用 构造复杂带 半封闭构造 地下水迟缓交替带 |
| 文章编号： | 1005-9539(2000)03-0308-04 |
| 修稿时间： | 1999年8月30日 |
The characteristics and formation causes of the geothermal water in Well H5 of Emeishan City in Sichuan |
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| QI Chun mei,XIAN Heng lin.The characteristics and formation causes of the geothermal water in Well H5 of Emeishan City in Sichuan[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2000,27(3):308-311. |
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| Authors: | QI Chun mei XIAN Heng lin |
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| Abstract: | Based on the analysis and research of the geological, hydrogeological and hydrochemical characteristics of Well H5, this paper holds that in the complicated and neotectonic intense terrain, atmospheric water percolates downwards, mixes itself with a small amount of sedimentary water after its deep circulation and leaching effect and becomes geothermal water. It is a deep circulation kind of middle or low temperature geothermal water under the control of fractures. |
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| Keywords: | karst groundwater leaching effect complicated tectonic zone hemiclosed structure alternate belt of gronud slug flow |
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