南京汤山温泉形成条件探讨  

The research on formation condition of Tangshan warm spring in Nanjing

作　　者：李爱勇[1] 朱春生[1] 杨生[2] 

机构地区：[1]江苏省有色金属华东地质勘查局八一四队,镇江212005 [2]有色金属矿产地质调查中心北京中色物探有限公司,北京100073

出　　处：《矿产勘查》2010年第6期546-549,共4页Mineral Exploration

摘　　要：汤山温泉为穹顶剥露的碳酸盐岩层间水,顶盖有良好的页岩屏蔽,深部有大地电磁测深(MT)探知的花岗岩体为热源,位于背斜与断裂发育的有利部位。Tangshan warm spring is formed by carbonate layer water which fornix roof is denuded. Its top is shielded full by shale rock and its deep exists heat source, granite bodies, which are explored by Magnetotelluric method （MT） and lie in favorable parts where anticline and fracture is growing.

关 键 词：温泉 碳酸盐岩 大地电磁测深 热源 南京 

分 类 号：P641.11[天文地球—地质矿产勘探] P314.1[天文地球—地质学]