摘要
白云鄂博矿区“白云岩”可以划分成“层状”磷灰石白云石碳酸岩，“层状”细粒稀土白云石碳酸岩、高硅白云石碳酸岩、低硅白云石碳酸岩、方解石碳酸岩等多种类型。它们是同一岩浆源不同演化阶段的产物。这些不同类型碳酸岩所携带的成矿物质，造就了白云鄂博矿床。
Baiyunebo deposit area "dolomitite"can be divided into many types,such as the "stratified"apatite fine rare, high-silica,low-silica dolomite carbonatite and calcspar carbonatite. They belong to same magmatic hearth of different types carbonatite intruded into the mineral-forming material of carrying then formed Baiyunebo mine.
出处
《内蒙古地质》
1997年第1期49-59,共11页
Geology of Inner Mongolia
