内蒙古赤峰市热水镇地热田地球物理调查  

Geophysical survey of the geothermal field in Reshuizhen of Chifeng city,Inner Mongolia

作　　者：石卓[1] 金旭[1] 管彦武[1] 陈晓冬[1] 

机构地区：[1]吉林大学地球探测与信息技术学院,长春130026

出　　处：《地球物理学进展》2010年第6期2168-2173,共6页Progress in Geophysics

基　　金：国家自然科学基金(40974047)资助

摘　　要：热水镇热构造背景具有略厚的地壳,稍低的大地热流和壳内相对的低温的特征.本区不具备浅部形成高温热源的火山地质背景.从西、北部山区渗透的天水,在深部被晚期侵入的花岗岩和玄武岩以热传导的形式加热,再沿发育的的断裂、裂隙上升到浅部形成地热田浅层热水储集层.地热田具有向北西—南东和南西—东北东方向伸展的趋势.There is no geological background of high temperature volcanic heat resources in Reshuizhen, Chifeng, Inner Mongolia, China, because of thicker crust, lower terrestrial heat flow and lower temperature in the crust. The water penetrated from the mountains in the north and west is heated by heat conduction at depth by the invaded granite and basalt. And the water rises up to the shallow reservoir along the ruptures. The geothermal field extends in northwest-southeast and southwest-northeast direction.

关 键 词：热构造背景 玄武岩火山活动 断裂构造 地球物理调查 热结构模型 

分 类 号：P631[天文地球—地质矿产勘探]