| 浅谈乌拉山金矿带金矿化类型 |
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| 引用本文： | 郎殿有.浅谈乌拉山金矿带金矿化类型[J].地质与资源,1997,6(3):193-198. |
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| 作者姓名： | 郎殿有 |
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| 作者单位： | 内蒙古包头市哈德门金矿 |
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| 摘 要： | 乌拉山金矿带金矿化分为石英脉型(Ⅰ),石英脉-蚀变岩型(Ⅱ),蚀变岩型(Ⅲ)三大类型,其分带性与大桦背花岗岩具有密切空间关系.
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| 关 键 词： | 乌拉山金矿带 金矿化系列类型 大华背花岗岩 内蒙古 |
| 收稿时间： | 1997-01-02 |
CLASSIFICAITON OF GOLD MINERALIZATION IN WULASHAN GOLD DEPOSIT BELT |
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| Lang Dianyou.CLASSIFICAITON OF GOLD MINERALIZATION IN WULASHAN GOLD DEPOSIT BELT[J].Geology and Resources,1997,6(3):193-198. |
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| Authors: | Lang Dianyou |
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| Institution: | Hademen Gold Mine, Baotou, Inner Mongolia |
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| Abstract: | Wulashan gold deposit belt,situated in the middle section of the north margin of North China platform,can be divided into 3 mineralization types,i.e.,quartz vein type (I),quartz vein altered rock type(Ⅱ) and altered rock type(Ⅲ).Each type can be subdivided into 2 sub types.The origin of the belt is closely related to Dahuabei granite body.The quartz vein type mineralization is located near the contact zone,01～05km to the granite.The quartz vein altered rock type is distributed along the outer of the contact zone,15～2km to the granite.The altered rock type is 3～6 km to the granite.The type Ⅱ and type Ⅲ are with great potential.Especially,the quartz vein altered rock sub type and the complex altered rock sub type have formed economic lodes. |
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| Keywords: | Wulashan gold deposit belt mineralization type granite Inner Mongolia |
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