| 山西省代县碾子沟金红石矿的成因分析 |
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| 引用本文： | 马雄华.山西省代县碾子沟金红石矿的成因分析[J].太原科技,2007,165(10):75-76. |
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| 作者姓名： | 马雄华 |
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| 作者单位： | 山西省晋中市榆次区鸣李三勘院地质勘察一分院,山西,晋中,030620 |
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| 摘 要： | 金红石在基性岩中是由于自变质作用和后期热液作用的结果,使矿体中金红石加富,该区矿床属岩浆矿床。介绍了代县碾子沟矿区金红石矿产的地质特征,就代县碾子沟矿区金红石矿的成矿原因进行了分析。
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| 关 键 词： | 代县碾子沟 金红石 成因 |
| 文章编号： | 1006-4877（2007）10-0075-02 |
| 收稿时间： | 2007-08-26 |
| 修稿时间： | 2007-09-05 |
Analyze the Cause of Rutile Ore in Nianzigou, Dai County, Shanxi Province |
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| Ma Xionghua.Analyze the Cause of Rutile Ore in Nianzigou, Dai County, Shanxi Province[J].Taiyuan Science and Technology,2007,165(10):75-76. |
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| Authors: | Ma Xionghua |
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| Institution: | Ma Xionghua |
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| Abstract: | In the radicel rock,rutile's formation is due to the metamorphism and the function of hydrotherm making the rutile rich in the orebody,and this deposit belongs to magmatic deposit.Introduce the geological features of rutile mineral in Nianzigou,Dai county,and analyze the reason of the rutile's formation in this mining area. |
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| Keywords: | Nianzigou Dai county rutile the reason of formation |
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