安徽淮河流域平原区地下水水温分布特征  

Groundwater temperature distribution features for the plains in the Huai River basin,Anhui

作　　者：杨佩明[1] 杨则东[1] 焦团理[1] 

机构地区：[1]安徽省地质调查院,安徽合肥230001

出　　处：《安徽地质》2012年第2期136-138,共3页Geology of Anhui

摘　　要：介绍了安徽淮河流域平原区第四纪地质与水文地质概况,通过对所采集的1362组地下水水温数据空间分布特征的分析,认为本地区地下水水温西高东低;蒙城、凤台—寿县—长丰一带和界首—亳州、砀山等地是寻找面源型地热资源的有利地区。This paper introduced the Quaternary geology and hydrogeology of the plains in the Huai River basin, Anhui. Based on analysis of spatial distribution features of sampled 1362 sets of groundwater temperature data, it is suggested that the groundwater temperature is higher in west and lower in east, and the potential surface source geothermal resources lie in the areas as Mengcheng, Fengtai-Shouxian-Changfeng, Jieshou-Bozhou and Dandangshan.

关 键 词：淮河流域 平原 地下水 水温 地热 安徽 

分 类 号：P641.12[天文地球—地质矿产勘探]