摘要
矿泉水赋存于沁水向斜北部东翼三叠系砂页岩地层中，１９８７年和１９９３年经山西地矿局和地矿部组织鉴定，水质符合《饮用天然矿泉水》国家标准（ＧＢ８５３７－８７），属含锶－偏硅酸重碳酸－钠钙型矿泉水。Ｙｈ＿１、井、Ｋ＿１井均已开发利用，生产瓶装天然矿泉水和矿泉水系列饮料。
The mineral water occurs in sandshale of Triassic system,structurally near the east-limb of the north part Qinshui syncline,In 1987 and 1993,respectively,the water qualityhad been identified by Shanxi Bureau of Geology & Mineral Resources and Ministry of Geolo-gy & Mineral Resources,It is accordant with national standard of《Potable Natural Mineralwater》(GB 8537-87), and belongs to strontium bearing-metasilicate,bicarbonate-sodiumcalcium type mineral water.Both well YH_1 and well K_1 have been mined and utilized andhave produced mineral water and a series of mineral water drinks.
关键词
锶-偏硅酸
矿泉水
水质特征
形成条件
strontium and metasilicate natural mineral water,Triassic System,Xiyaoof Yuci
