摘要
峨眉山是中国著名的风景旅游区，区内有３０°Ｃ左右的温泉出露，富含氡气。文章重点介绍了峨眉山柿子坪热田的地表热异常区发育特征，以及与之有关的深部地下水排泄和断裂构造特征。
Emei Shan is a well known tourist resort of China. There are hot springs which contain Rn and thier temperatures are about 30°C. So the study and exploration of the geothermal water in the area have been concerned . Based on a series of studies made by the author in 1997, the author found the Shiziping geothermal field. In this paper , the characteristics of the ground geothermal anomaly, deep groundwater drainage amd geological structure of the field are disscussed.
出处
《成都理工学院学报》
CSCD
1999年第1期58-63,共6页
Journal of Chengdu University of Technology
关键词
峨眉山
地热田
地表热异常
地下热水
geothermal field
Emei Shan
ground geothermal anomaly
