摘要
在分析老子山地热矿区地质背景、水文地质条件、地球物理特征和地球化学特征的基础上,认为本地区地热资源受构造裂隙控制,属于深循环成因的浅埋型中低温地下热水资源,具备了地热资源系统的覆盖层、热储层、热源以及传热通道等条件,为进一步勘查和开发老子山地热资源提供依据。
Based on the analysis of geological background, hydrogeological conditions, geochemical and geophysical characteristics of the Laozi Mountain geothermal mining area, it is considered that in the Laozi Mountain geothermal mining area the geothermal resources are controlled by the structures, and the geothermal resources in the region are deep-cycle caused and the shallow type of mid to low-temperature geothermal water resources; Geothermal resources have cover, heat reservoir, heat sourse, heat transfer and access conditions, which will be the base of the further exploration and development of geothermal resources in Laozi Mountain mining area.
出处
《煤田地质与勘探》
CAS
CSCD
北大核心
2009年第2期47-50,54,共5页
Coal Geology & Exploration
关键词
地热矿区
地热资源
赋存特征
老子山地区
geothermal mining area
geothermal resources
occurrence features
Laozi Mountain area