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。
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.
出处
《云南地质》
2011年第1期67-70,共4页
Yunnan Geology
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
Far Supplement - Deep Cycle
Buried Hot Spring
Migration of Fault - Fracture Zone
Medicine Quality of Water
Changli, Yuxi, Yunnan