| 陕西省洛南地区铁金矿地质特征及找矿前景 |
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| 引用本文： | 崔辰亮,王晓娣,甄泽.陕西省洛南地区铁金矿地质特征及找矿前景[J].世界有色金属,2020(5):99-100. |
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| 作者姓名： | 崔辰亮 王晓娣 甄泽 |
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| 作者单位： | 中化地质矿山总局河北地质勘查院,河北 石家庄 050031;中化地质矿山总局河北地质勘查院,河北 石家庄 050031;中化地质矿山总局河北地质勘查院,河北 石家庄 050031 |
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| 摘 要： | 该矿区位于华北地矿南缘,矿区出露地层为中元古界长城系上熊耳群,以块状细碧岩为主,夹杏仁状细碧岩、泥砂质板岩、凝灰质板。分为上熊耳群中段、上熊耳群下段。翻山沟铁矿为熊耳群火山沉积作用、区域变质作用与后期构造热液复合叠加形成的铁矿床。
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| 关 键 词： | 铁金矿 地质特征 |
Geological characteristics and prospecting prospect of iron and gold deposits in Luonan area,Shaanxi Province |
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| CUI Chen-liang,WANG Xiao-di,ZHEN Ze.Geological characteristics and prospecting prospect of iron and gold deposits in Luonan area,Shaanxi Province[J].World Nonferrous Metals,2020(5):99-100. |
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| Authors: | CUI Chen-liang WANG Xiao-di ZHEN Ze |
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| Affiliation: | (Hebei Institute of geological exploration,Sinochem Bureau of Geology and mines,Shijiazhuang 050031,China) |
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| Abstract: | The mining area is located in the south margin of North China.The exposed strata of the mining area are the upper Xiong’er Group of the Great Wall System of the Middle Proterozoic,mainly composed of massive spilite,intercalated with amygdaloid spilite,argillaceous slate and tuffaceous plate.It can be divided into the middle part of the upper bear ear group and the lower part of the upper bear ear group.The fanshangou iron deposit is formed by the combination of volcanic sedimentation,regional metamorphism and later tectonic hydrothermal. |
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| Keywords: | iron gold deposit geological characteristics |
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