| 白云金矿床地质特征及成因探讨 |
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| 引用本文： | 赵鸿志,杨沈生,李辉. 白云金矿床地质特征及成因探讨[J]. 有色矿冶, 2009, 25(3): 4-7 |
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| 作者姓名： | 赵鸿志 杨沈生 李辉 |
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| 作者单位： | 辽宁省有色地质局106队,辽宁,铁岭,112001 |
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| 摘 要： | 白云金矿床位于青城子矿田外围，产出于白云推覆构造带中，围岩主要为辽河群盖县组的矽线石云母片岩和黑云母变粒岩。主要矿化类型为硅钾蚀变岩型。
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| 关 键 词： | 推覆构造 硅钾蚀变岩 矿床特征 成因探讨 |
Geologic Features of Baiyun Gold Ore Deposit and Discussion of the Genesis |
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| ZHAO Hong-zhi,YANG Shen-sheng,LI Hui. Geologic Features of Baiyun Gold Ore Deposit and Discussion of the Genesis[J]. Non-Ferrous Mining and Metallurgy, 2009, 25(3): 4-7 |
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| Authors: | ZHAO Hong-zhi YANG Shen-sheng LI Hui |
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| Affiliation: | (Liaoning Non--ferrous Tieling Geologic Exploration Institute Tieling Liaoning 112001) |
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| Abstract: | Baiyun gold ore deposit is located at the periphery of Qingchengzi mine field, occurring in Baiyun nappe structure belt, the wall rock is mainly the sillimanite mica schist and biotite of Liaohe groap Gaixian formation. The main mineralization category is silicon--potassium altered rock category. |
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| Keywords: | nappe structure silicon--potassium altered rock deposit feature discussion of the genesis |
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