| 东书院金矿地质特征及矿床成因初探 |
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| 引用本文： | 赵先平 衣德学. 东书院金矿地质特征及矿床成因初探[J]. 山东轻工业学院学报, 1994, 8(4): 68-72 |
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| 作者姓名： | 赵先平 衣德学 |
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| 作者单位： | 山东地矿局八队，山东轻工业学院无机材料系 |
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| 摘 要： | 东书院金矿是胶南隆起上第一个有工业价值的金矿床。矿体赋存于北东向的东书院断层内；断层内的闪长玢岩脉与矿体关系密切，常与金矿伴生；含金矿物主要是金银矿和银金矿两种，以粒间金为主，其次为裂隙金；矿床成因为蚀变岩型金矿床。
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| 关 键 词： | 成矿条件 地质特征 矿床成因 金矿 |
A Preliminary Study on the Geological Features and Genesis of Deposit of the Gold Ore in Dongshuyuan |
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| Zhao Xianping. A Preliminary Study on the Geological Features and Genesis of Deposit of the Gold Ore in Dongshuyuan[J]. Journal of Shandong Institute of Light Industry(Natural Science Edition), 1994, 8(4): 68-72 |
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| Authors: | Zhao Xianping |
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| Abstract: | Dongshuyuan gold deposit is the first deposit of industrial value,located inJiaonan Rise, The orebody exists in Dongshuyuan fault which extends east-northward.Thedioritic porphyrite vein existing in the fault is closely related with the orebody,and usuallyassociates with the gold deposit. The gold-bearing mineral mainly consists of goldargentidand electrum,with grain boundary gold mineral coming first,crevice gold mineral the second Genesis of the gold deposit is of altered rock type. |
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| Keywords: | mineral formation condition geological features genesis of deposit. |
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