摘要
根据位于河北邢台东部太行山前大断裂东侧的金地热1号井的水质化验资料和测温资料,邢东地热水为镭、硅、氟、硫酸钙钠型高热复合矿水,具有较好的医疗价值,为核试验之前降水而成;地热温度随埋藏深度而自然增高(埋深2900m时,井温89.9℃),其地热类型属于盆地型中低温地热资源。
According to water quality testing and temperature measuring data from JDR No.1 well located at east side of Taihang Mts. piedmont major fault in eastern Xingtai, Hebei, the geothermal water is radium, silicone, fluorine, SO4-Ca,Na type high temperature composite mineral water. The water has preferable medical value; it was formed before nuclear tests. Geothermal temperature is rising along with the deepening of the depth （well temperature is 89.9oC when it is 2900m in depth）, belongs to basin type medium to low temperature geothennal resource.
出处
《中国煤田地质》
2005年第5期50-51,57,共3页
Coal Geology of China
关键词
热矿水
奥陶系
热储
酸性硫酸水
邢台东部
hot mineral water
Ordovician System
geothermal resrvoir
acidic sulphate water
eastern Xingtai
