长岭凹陷潜在地热初步探讨  

Primary discussion on potential geotherm within Changling sag

作　　者：王洪涛[1] 赵向辉[1] 陈家林[2] 代丽霞[2] 陆浩[3] 陈殿义[1] 

机构地区：[1]吉林省地矿信息中心,吉林长春130061 [2]吉林省区域地质矿产调查所,吉林长春130022 [3]吉林省地矿勘察设计研究院,吉林长春130061

出　　处：《吉林地质》2009年第1期51-56,共6页Jilin Geology

摘　　要：根据长岭凹陷石油井地温测量和物探资料,从地热形成的4要素——储、盖、通、源以及地热具备的地质特征入手,分析了长岭凹陷潜在着地热资源。目前长岭盆地基本具备了储和盖,需要进一步寻找的是通和源。Potential geothermal resources within Changling sag is analysed on the basis of data both geotemperature survey in oil wells and geophysical prospecting, according to the four factors of geothermal existence, i.e., geothermal formation, geothermal confiding layer, offset structures, and water resource, geothermal resource. At present, there are geothermal formation, geothermal confiding layer within Changling sag, diversion water fissure and water resource, geothermal resource need finding further.

关 键 词：地热 储、盖、通、源 长岭凹陷 

分 类 号：P314.1[天文地球—固体地球物理学]