【摘要】 灵宝盆地热储分为层状热储和带状热储两种类型,层状热储又分为温水储层和温热水储层两个热储层。对灵宝盆地地下水的同位素进行了测试,结合大气降水线方程,对地下热水的补给来源和形成年龄进行了分析。结果表明:灵宝盆地地热水的成因为大气降水;地热水的补给来源为南部山区,补给区平均高程为577.82 m;地热水的年龄均在万年以上;地热水各热储层之间无明显的水力联系。更多还原

【Abstract】 It is divided into stratified reservoir and zoned reservoir in Lingbao basin.The stratified reservoir consists of warm water reservoirs and warm-hot water reservoirs.Based on the isotope test results of groundwater,it combined with Henan Province precipitation line equation and analyzed the recharge sources and formation age of geothermal water.The results showed that: atmospheric precipitation coming from south mountain is the main recharge source of groundwater.It’s average height is 577.82 m in the recharge area.Geothermal water’s age is over ten thousand years.There is no obvious hydraulic connection between each heat storage layer.更多还原