摘要
新田县富锶矿泉水分布面积约176.7km2,赋存地层为泥盆系佘田桥组。本文分析了富锶矿泉水形成的地质、水文地质条件,同时分析了机井与下降泉锶含量差异的受控因素。
The distribution area of rich strontium mineral water is about176.7 km2 in Xintian county,and present in the strata of D3 s .The geological and hydrogeological conditions of the formation of rich strontium mineral water are analyzed,and the difference of controlling factor between the well and the spring is analyzed.
作者
苏春田
罗飞
杨杨
巴俊杰
李小盼
SU Chuntian;LUO Fei;YANG Yang;BA Junjie;LI Xiaopan(Institute of Karst Geology,CAGS/Key Laboratory of Karst Dynamics,MNR&GZAR,Guilin 541004,China)
出处
《中国矿业》
北大核心
2019年第A01期347-348,共2页
China Mining Magazine
基金
中国地质调查局地质调查项目“南北盘江流域水文地质调查”资助(编号:DD20190342)
关键词
新田县
岩溶
富锶矿泉水
形成机理
Xintian county
karst
rich strontium mineral water
formation mechanism
