摘要
山西饮用天然矿泉水资源丰富。目前已对５５处矿泉水进行了勘查评价。矿泉水的分布受活动性断裂构造和新生代断陷盆地控制，一般见于盆地边山和平原，主要分布在新生界的松散层内（３２．７３％），其次为中生界、古生界的碎屑岩（２２．９２％）和碳酸盐岩（２７．２７％）地层中。各岩类中矿泉水的达标元素和组分主要是锶，其次是偏硅酸。地热异常区的饮用天然矿泉水资源也很丰富，但一些热水中含氟超过国家标准。
Shanxi potable natural mineral water is rich in natural resources.At present,55 springsof mineral water has been carried on exploration and assessment.The distribution of mineralwater is under the control of active faulted structure and fault basin of Cenozoic Era.Themineral water is generally distributed in the margin of basin and plain, and primarily in loosebed of Cenozoc Erathem(32.73%),and the secondly in detrital rock(22.92%)and Carbonaterock(27.27%)of Mesozoic Erathem and Pa1aeozoic Erathem. The attained element and com-ponent of mineral water of various rock is main Sr-bearing and secondly metasilicate. The re-sources of potable natural mineral water is also abundant in geothermal anomaly regions,butcontent of fluorine is exceed national standard in some thermal water.
关键词
饮用
天然矿泉水
地下热水
分布特征
potable natural mineral water,fault basin, underground thermal water,Shanxi province
