| 鹰嘴山西铁锰矿地质特征及找矿方向 |
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| 引用本文： | 杨彦义,豆小刚,亢松松,白亮.鹰嘴山西铁锰矿地质特征及找矿方向[J].甘肃冶金,2014(4):60-64. |
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| 作者姓名： | 杨彦义 豆小刚 亢松松 白亮 |
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| 作者单位： | 甘肃省有色金属地质勘查局张掖矿产勘查院,甘肃张掖734012 |
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| 摘 要： | 本文阐述了鹰嘴山西铁锰矿地层、构造、侵入岩、矿体及围岩蚀变特征,指出了鹰嘴山西铁锰矿床位于阿尔金走滑断裂的南东侧、鹰嘴山向斜南翼,成矿构造地质环境复杂,构造活动强烈,岩脉走向受断裂控制明显,为矿液的运移富集提供了热源。本文着重论述了矿床地质特征及控矿因素,并对矿床成因进行了初步分析,提出了一定的找矿方向。
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| 关 键 词： | 地质特征 矿床成因 控矿因素 找矿方向 |
Geological Characteristics and Prospecting Direction of Iron Deposit in The West of Yingzuishan |
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| YANG Yan-yi,DOU Xiao-gang,KANG Song-song,BAI Liang.Geological Characteristics and Prospecting Direction of Iron Deposit in The West of Yingzuishan[J].Gansu Metallurgy,2014(4):60-64. |
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| Authors: | YANG Yan-yi DOU Xiao-gang KANG Song-song BAI Liang |
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| Affiliation: | (Zhangye Ceo-Min Surven Institute of Non-Ferrous Metal Geological Exploration Burean of Gansu Province, Zhangye 734012, China) |
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| Abstract: | The stratum, tectonic, intrusive rock, ore body and host-rock alteration of iron deposit in the west of Yingzuis-han are explained .The iron deposit is located in the southeast of Altun Tagh fault zone and in the south of Yingzuishan syncline.The metallogenic tectonic environment is complex , the tectogenesis is strong, and the fracture controlled the strike of dike, so it supplied heat source for oresolution’s migration and concentration.Emphasis is placewd on the deposit’s geological characteristics and orecontrol factor, and analysis on the deposit ’s origin, and finally a few prospecting direction is introduced . |
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| Keywords: | geological feature genesis of mineral deposit ore-controlling factors prospecting direction |
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