浅析阿尔山地热地质特征  

The geothermal geological features of Arxan mountains

作　　者：祁福利[1,2] 张峰龙[3,2] 鲁守刚[3,2] 孙永泉[3,2] 

机构地区：[1]吉林大学建设工程学院,吉林长春130026 [2]黑龙江省九○四水文地质工程地质勘察院,黑龙江哈尔滨150027 [3]吉林大学环境与资源学院,吉林长春130026

出　　处：《吉林地质》2012年第2期109-112,共4页Jilin Geology

摘　　要：从阿尔山地热区域地质演化、地热地球物理特征、地热成控条件等方面进行研究,认为该区地热资源的主要断裂构造,为内蒙—大兴安岭地槽褶皱系的中段,其中金江沟、银江沟、五里桥热储构造带上地幔的岩浆向上运移的通道为哈拉哈河岩石圈断裂和NNW向基底断裂。Through the research the geothermal of the regional geological evolution,geothermal geophysical features,geothermal control condition in Arxan Mountains.It is considered that the major fracture structure of the geothermal resources is the middle part of the geosynclinal folded system of Inner Mongolia-Daxinganling.Among them,Jinjianggou,Yinjianggou,Wuliqiao thermal reservoir tectonic belts,The channel,which of upper mantle magma upward migration,is the Halha river lithospheric fracture and NNW strike basilar fracture.

关 键 词：阿尔山 地热资源 地质特征 

分 类 号：TK521[动力工程及工程热物理—热能工程]