广西新寨矿泉水出露特征及形成机理  

OUTCROP FEATURES AND GENETIC MECHANISM OF THE MINERAL WATER IN XINZHAI,GUANGXI PROVINCE

作　　者：张茂忠[1] 周奇明[1] 李水明[1] 屠惠民 区杏 

机构地区：[1]中国有色金属工业总公司矿产地质研究院

出　　处：《矿产与地质》1996年第2期114-119,共6页Mineral Resources and Geology

摘　　要：新寨矿泉水属重碳酸钙钠型低钠、低矿化度的含氡硅酸矿泉水，是来自花岗岩体中较深层的构造裂隙水，其水质、水量、水温十分稳定，为花岗岩体中较深层的构造裂隙水。矿泉水中有益元素的物质组份来源于花岗岩体，偏硅酸和氡含量达到国家标准。The mineral water in Xinzhai is a calcium sodium bicarbonate kind of radon bearing mineral water with low sodium and degree of mineralization, which is from deeper, structural feasures in granite. Its quality, quantity and temperature are very stable, The components of beneficial elements in the water are from the granite. Contents of partial silica and radon accord with the standard of the State. Therefore it has economic values.

关 键 词：矿泉水 水化学 出露特征 形成机理 

分 类 号：P641.5[天文地球—地质矿产勘探]