摘要
在一些地区经常会有地热水冒出,为研究热涌出点的形成原因,本文根据专项水文地质勘查成果,结合工程物探及钻探等手段,初步分析平果铝3#排泥库区域深部地热地质条件,基本查明区内热储和盖层的分布、产状、岩性、厚度和埋深,断裂的产状、规模、力学性质和导热性,以及区内地温梯度特征等地热成生条件。为该地区热储地质研究初步探明方向及开发利用地热资源积累了重要数据。
Geothermal water often emerges in some areas.In order to study the cause of the formation of the heat gushing point,this paper,based on the results of special hydrogeological exploration,combined with engineering geophysical prospecting and drilling and other means,preliminarily analyzes the deep geothermal geological conditions of Pingguo Aluminum 3 # mud dump area,and basically finds out the distribution,occurrence,lithology,thickness and burial depth of the thermal reservoir and cap rock in the area,as well as the occurrence,scale,mechanical properties and thermal conductivity of the fault,And geothermal generation conditions such as temperature gradient characteristics in the region.It has accumulated important data for the preliminary direction of thermal reservoir geological research and the development and utilization of geothermal resources in this area.
作者
覃满满
邓忠
QIN Man-man;DENG Zhong(Guangxi Institute of Hydrogeology and Engineering Geology Survey,Liuzhou 545006,China)
出处
《价值工程》
2023年第26期120-122,共3页
Value Engineering
关键词
地热系统
地热储
地热增温率
盖层
geothermal system
geothermal reservoir
geothermal gradient
cap rock
