翁牛特旗——库伦旗一带严重缺水区的地质环境及找水途径  

Geological Environment and Water-Finding Approach in the Areasfrom Wongniuteqi to Kulunqi Where Short of Water Seriously

作　　者：高秀花[1] 龙文华[2] 殷淑华[1] 段青梅[1] 

机构地区：[1]中国地质大学水资源与环境学院,北京100083 [2]内蒙古自治区地质调查院

出　　处：《地下水》2005年第2期131-135,共5页Ground water

摘　　要：翁牛特旗——库伦旗一带为西辽河平原周边的严重缺水区。通过分析研究区地下水形成的地质环境,认为降水量、地形地貌、岩性构造和地下水循环是造成研究区严重缺水的主要因素,地层岩性和新构造运动是影响地下水富集的决定性因素。指出要加强含水层的岩性和构造、基岩区的断裂性质和产状的研究,并提出在基岩区、低山丘陵区寻找构造裂隙水和断裂带脉状水是解决研究区严重缺水的较好途径。Circumjacent area of west Liaohe River campagna from Wongniuteqi to Kulunqi is Short of Water Seriously. The article thinks the main causes is precipitation, landform and geomorphy, lithology structure and groundwater circulation which result in the area short of water seriously by analyzing geological environment of groundwater formation. The stratum lithology and new structure movement are the crucial factors that influence groundwater environment. And it points out to strengthen the study on lithology and structure of the aquifer and fracture character and forming situation of bedrock area, and puts forward the better approach to solve the problem of serious water shortage that is searching structural crevice water and fracture zone vein water in the bedrock and low-relief terrain hilly area.

关 键 词：翁牛特旗 库伦旗 地质环境 严重缺水区 降水量 地形地貌 岩性构造 地下水循环 

分 类 号：P641.72[天文地球—地质矿产勘探]