| 玉溪常里温泉成因探讨 |
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| 引用本文： | 宋子德.玉溪常里温泉成因探讨[J].云南地质,2011,30(1):67-70. |
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| 作者姓名： | 宋子德 |
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| 作者单位： | 云南省地质调查院区域地质调查所,云南,玉溪,653100 |
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| 摘 要： | 常里温泉处于普渡河断裂与大密罗-马官屯断裂交汇带,地质构造条件特殊,地下水循环较复杂.温泉水温高、水质好、埋藏浅、易开采、交通方便等优势,具有较高的开发价值.温泉形成机理,补、径、排循环系统的研究,有助于科学、合理指导开发利用温泉资源.
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| 关 键 词： | 远补给深循环 隐伏型温泉 断裂破碎运移 医用水质 云南玉溪常里 |
A DISCUSSION ABOUT THE GENESIS OF CHANGLI HOT SPRING IN YUXI |
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| SONG Zi-de.A DISCUSSION ABOUT THE GENESIS OF CHANGLI HOT SPRING IN YUXI[J].Yunnan Geology,2011,30(1):67-70. |
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| Authors: | SONG Zi-de |
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| Institution: | SONG Zi-de(Regional Geology Survey,Yunnan Institute of Geological Survey,Yuxi 653100) |
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| Abstract: | The Changli hot spring is in the intersection zone of Puduhe fault and Damiluo-Maguantun fault, with the special geology - structure conditions and complicated underground water cycle. Because of the superiority of high T, good water quality, shallow buried depth, easy exploitation and convenient traffic, the development significance is very great. The study on genesis mechanism, cycle system of supplement, surface flow and drainage is very helpful in the scientific and rational direction of exploitation and utilization of the hot spring resources. |
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| Keywords: | Far Supplement-Deep Cycle Buried Hot Spring Migration of Fault-Fracture Zone Medicine Quality of Water Changli Yuxi Yunnan |
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