北京市近郊锶型矿泉水带的发现

Discovery on the Sr-type mineral water zone in Beijing outskirts

北京地区埋藏着一条自西向东锶含量高、水量丰富的锶型矿泉水富水带。该矿泉水带主要赋存在奥陶系灰岩、体罗系洼里砾岩以及部分第四系含水层中,在地质构造上受断裂所控制。

There is a Sr-type mineral water zone with high-content Sr element and abundant water content,which is buried from the west to east in Beijing outskirts.This zone occurs mainly within Ordovician limestones,Jurassic Wali Formation conglomerates,and Quaternary aquifers.Tectonically, it is controlled by the fractures and faults.