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白云鄂博矿区周围火成碳酸岩岩墙地质特征
引用本文:陶克捷,王文志.白云鄂博矿区周围火成碳酸岩岩墙地质特征[J].地质科学,1998,33(1):73-83.
作者姓名:陶克捷  王文志
作者单位:1. 中国科学院地质研究所, 北京 100029;2. 包头钢铁公司矿山研究所, 包头 014010
摘    要:首次填出白云鄂博矿区周围火成碳酸岩岩墙的分布图,深入系统地研究了岩墙的地质产状、主矿物类型、岩石结构、人工重砂矿物组成、稀土元素含量等特征。反映了白云鄂博矿区周围火成碳酸岩岩墙的岩浆演化分异过程存在差异。对于研究白云鄂博矿区铁与稀土的矿化提供了物质来源的证据。

关 键 词:火成碳酸岩岩墙  方解石  白云石  岩石结构  稀土元素  白云鄂博
收稿时间:1997-03-21
修稿时间:1997-03-21;

SYSTEMATIC GEOLOGICAL INVESTIGATION ON CARBONATITE DYKES IN BAYAN OBO, INNER MONGOLIA, CHINA
Tao Kejie,Yang Zhuming,Zhang Peishan,Wang Wenzhi.SYSTEMATIC GEOLOGICAL INVESTIGATION ON CARBONATITE DYKES IN BAYAN OBO, INNER MONGOLIA, CHINA[J].Chinese Journal of Geology,1998,33(1):73-83.
Authors:Tao Kejie  Yang Zhuming  Zhang Peishan  Wang Wenzhi
Institution:1. Institute of Geology, Chinese Academy of Sciences, Beijing 100029;2. Institute of Mining, Baotou Iron and Steel Corporation, Baotou 014010
Abstract:The geological map showing distribution of carbonatite dykes around the Bayan Obo Nb-REE-Fe mine was firstly presented.A systematic study on occurrence,mineralogical type,rock texture,mineral component and REE content of those carbonatite dykes has been carried out.The results indicate that there existed differences of magmatic evolution during the formation of those carbonatite dykes.It implicates that the carbonatite magma may be a source for Nb-REE-Fe mineralization of the Bayan Obo deposit.
Keywords:Carbonatite dyke    Calcite  Dolomite    Texture  Rare earth  Bayan Obo  
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