贵州思南温泉的成因分析  

Study on the Origin of Sinan Hot Springs in Guizhou Province

作　　者：钟响[1,2] 杨鹏程[1] 杨文亮[1] 

机构地区：[1]贵州省地质矿产勘查开发局111地质大队,贵州贵阳550008 [2]中国地质大学(武汉)环境学院,湖北武汉430074

出　　处：《山东国土资源》2015年第10期40-43,共4页Shandong Land and Resources

摘　　要：通过地质分析,借助可控源音频大地电磁测深物探手段,认为思南温泉补给源来自其西部沙沟向斜核部热水沿樱桃断裂带上升,并在鹦鹉溪背斜核部岩体破碎带排泄出地表。通过对贵州思南温泉水样的水质分析,采用地球化学温标法研究了思南温泉的热储温度为53℃,并研究得出热水循环深度为1 500 m。Through geological magnetotelluric sounding, it is analysis and geophysical research, by means of controlled source audio frequency regarded that Sinan hot spring recharge source is from the hot water rising along Yingtao fault zone in the core area of Shagou syncline in its western part. It excrets from the fracture zone in the core of Yingwuxi anticline to the surface. Through water quality of water samples of Sinan hot spring in Guizhou province, by using geothermometer method, it is regarded that heat reservoir temperature is 53℃, and the hot wa- ter cycle depth is 1159m.

关 键 词：思南温泉 水质分析 热储温度 循环深度 贵州 

分 类 号：P314.1[天文地球—固体地球物理学]