| 内蒙古大扬气西钼矿体地质特征及成因分析 |
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| 引用本文： | 苏航,李中会,宋丙剑. 内蒙古大扬气西钼矿体地质特征及成因分析[J]. 甘肃冶金, 2016, 0(6). DOI: 10.3969/j.issn.1672-4461.2016.06.019 |
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| 作者姓名： | 苏航 李中会 宋丙剑 |
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| 作者单位： | 1. 黑龙江省地质调查研究总院齐齐哈尔分院,黑龙江 哈尔滨,150036;2. 武警警种学院,北京,102202 |
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| 摘 要： | 通过对内蒙古大扬气西钼矿体地质背景及地质、地球物理与地球化学特征的研究,建立成矿模型。本次共圈出矿体四条,矿体呈脉状,走向近南北向,最高品位0.128%,属与流纹岩有关热液型矿床。
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| 关 键 词： | 钼矿体 热液型 大扬气 |
Geological Features and Cause Analysis of Mo Ore Body In the Western Dayangqi,Inner Mongolia |
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| Abstract: | Through study on the geological background and geological, geophysical and geochemical features of the Western Dayangqi molybdenum deposit in Inner Mongolia, and the metallogenic model was set up. Four ore bodies were delineated. The ore bodies are vein-shaped with north-south strike, and the highest grade of the deposit is 0.128%, belonging to the hy-drothermal type deposit related to the rhyolite. |
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| Keywords: | molybdenum ore body hydrothermal type Dayangqi |
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