| 四川盐边红格温泉成因研究 |
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| 引用本文： | 刘明富.四川盐边红格温泉成因研究[J].中国煤炭地质,2008,20(3):45-48. |
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| 作者姓名： | 刘明富 |
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| 作者单位： | 刘明富（四川省煤田地质局141队,四川,德阳,618000） |
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| 摘 要： | 针对红格温泉所处的地层、地质构造、水文地质条件，结合该区域地热背景分析了红格温泉的成矿条件，研究区内深度已达上地幔的昔格达深大断裂深部热源，区内发育的断裂构造及其断裂破碎带，厚约200m的昔格达组砂、泥、页岩互层的良好隔热盖层，区内丰富的大气降水、地表水与岩溶水资源，区内地热水产出的最低侵蚀基准面（沿崖羊河谷发育的清门口断裂带），为红格温泉的形成提供了良好的物资基础。
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| 关 键 词： | 温泉 成因研究 深部热源 储热构造 隔热盖层 水文地质特征 红格温泉 |
| 文章编号： | 1674-1803(2008)03-0045-04 |
| 修稿时间： | 2007年1月4日 |
A Study on Genesis of Hongge Hot Spring in Yanbian, Sichuan Province |
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| Liu Mingfu.A Study on Genesis of Hongge Hot Spring in Yanbian, Sichuan Province[J].Coal Geology of China,2008,20(3):45-48. |
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| Authors: | Liu Mingfu |
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| Institution: | Liu Mingfu (No.141 Exploration Team, Sichuan Bureau of Coal Geological Exploration, Deyang, Sichuan 618000) |
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| Abstract: | Expounded strata, structure and hydrogeological condition of the Hongge hot spring lies in, combined with regional geothermal setting analyzed hot spring forming conditions. The upper mantle reached Xigeda major fault is the heat source; well developed faults and fracture zone the thermal channel; about 200m thick Xigeda Formation alternating sandstone, mudstone and shale as the good heat insulating cap rocks; abundant atmospheric precipitation, surface water and karstic water as the water sources and heat water outcropping lowest base level of erosion （Qingmenkou fracture zone developed along the Yayang River） are all provided favorable material basis for the forming of Hongge hot spring |
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| Keywords: | hot spring genesis study deep heat source heat-storage reservoir structure heat insulating cap rock hydrogeological features Hongge hot spring |
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