| 山西大同六亩地一带石墨成矿地质特征 |
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| 引用本文： | 刘福生.山西大同六亩地一带石墨成矿地质特征[J].西南科技大学学报,1990(2). |
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| 作者姓名： | 刘福生 |
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| 作者单位： | 山西省建材科研所 |
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| 摘 要： | 本文论述了大同六亩地一带石墨地质特征,从固定CO_2,CaO和MgO的分析对比,论证了碳质来源于碳酸盐岩石,并提出构造、岩相对成矿的控制作用。得出石墨矿床属混合岩化区域变质型的结论。
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| 关 键 词： | 石墨 矿床 变质岩 |
The Geological Characteristics of Graphite Mineralization in Liumude Area, Datong, Shanxi |
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| Liu Fusheng.The Geological Characteristics of Graphite Mineralization in Liumude Area, Datong, Shanxi[J].Journal of Southwest University of Science and Technology,1990(2). |
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| Authors: | Liu Fusheng |
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| Institution: | Shanxi Research and Design Institute of Biulding Materials |
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| Abstract: | The geological characteristics of graphite mineralization is discussed in this paper. According to the analyses of C, CO2 and MgO Compostions, it is comfirmed that carbon comes from the carbonate rock and graphite mineralization is controlled by the structure litho-facies. The conclusion that graphite deposit belongs to bhe migmati zation regional metaomorphic graphite deposit is dracon. |
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| Keywords: | graphite deposit metamorphic rock |
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