| 白云鄂博矿区“白云岩”成因的初步研究 |
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| 引用本文： | 张建生,雷瑞英.白云鄂博矿区“白云岩”成因的初步研究[J].内蒙古地质,1997(1). |
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| 作者姓名： | 张建生 雷瑞英 |
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| 作者单位： | 内蒙古地勘局地研所 |
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| 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。
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| 关 键 词： | 白云鄂博 碳酸岩 |
Study "Dolomitite"Genesis of Baiyunebo Deposit Area |
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| Zhang Jiansheng,Lei Ruiying.Study "Dolomitite"Genesis of Baiyunebo Deposit Area[J].Geology of Inner Mongolia,1997(1). |
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| Authors: | Zhang Jiansheng Lei Ruiying |
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| Institution: | Inner Mongolia institute of geology |
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| Abstract: | 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. |
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| Keywords: | Baiyunebo carbonatite |
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