浅析南京六合地区形成地热的有利条件  

Analysis of forming geothermal favorable conditions in Liuhe area of Nanjing city

作　　者：丁梅花[1,2] 朱春生[2] 

机构地区：[1]江苏省有色金属华东地质勘查局,江苏南京210093 [2]江苏省有色金属华东地质勘查局八一四队,江苏镇江212005

出　　处：《地下水》2016年第1期22-24,共3页Ground water

摘　　要：地热资源是埋藏在地下一定深度范围内、可开采且经济环保的可再生能源,是现阶段重要的绿色能源之一。南京六合地区位于冶山—汤泉复式背斜的北端,断裂发育,重力梯度带贯穿其间,与香泉、汤泉具有相似的温泉形成机制及水文地质条件,自身具有得天独厚的地质条件,能为地下水上移提供良好通道和热源并与之呈带分布,具有良好的地热地质条件与开发远景。Geothermal resources are buried in the ground within the scope of a certain depth,which are recoverable,economic and renewable energy,and is one of the important green energy recently. For Liuhe area of Nanjing city,it is located in the northern end of Tangquan- Yeshan duplex anticline,where are lots of faults,and there is a gravity gradient belt across the area. And the forming mechanism of hot springs and hydrogeology conditions in Liuhe are similar to Xiangquan spring and Tangquan spring,and they are distributed in the same belt. Therefore,there are good geothermal geological conditions and developing prospect in Liuhe area.

关 键 词：地热资源 复式背斜 水文地质条件 重力梯度带 

分 类 号：P314.1[天文地球—固体地球物理学]