湖北省大冶市叶家庄矿区铜多金属矿成矿地质特征及下步找矿方向 |
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引用本文: | 聂振邦,余兴江,黄婉,姜明宇,孙达,徐新安. 湖北省大冶市叶家庄矿区铜多金属矿成矿地质特征及下步找矿方向[J]. 资源环境与工程, 2021, 35(2): 157-161 |
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作者姓名: | 聂振邦 余兴江 黄婉 姜明宇 孙达 徐新安 |
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作者单位: | 湖北省地质局 第一地质大队,湖北 大冶 435100 |
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基金项目: | 湖北省地质勘查基金项目——湖北省大冶市叶家庄—东角山矿区外围铜多金属矿补充普查(〔2020〕2号)。 |
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摘 要: | 叶家庄铜多金属矿区的矿体受阳新岩体石英正长闪长岩与碳酸盐岩围岩接触带控制,主要赋存于接触带矽卡岩和近接触带蚀变岩体中.矿床与燕山期石英正长闪长岩浆活动有紧密成因联系.石英正长闪长岩与碳酸盐岩接触带是寻找铜多金属矿的有利部位,矽卡岩化和硅化是重要的找矿标志.通过类比周边矿床认为,叶家庄矿区北西向接触带及深部有扩大矿床规模...
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关 键 词: | 铜多金属矿 阳新岩体 地质特征 找矿方向 叶家庄 |
Geological Characteristics and Prospecting Direction of Yejiazhuang Copper-Polymetallic Deposits Area in Daye City,Hubei Province |
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Affiliation: | (First Geological Brigade of Hubei Geological Bureau,Daye,Hubei 435100) |
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Abstract: | The ore body in the Yejiazhuang copper-polymetallic mining area is controlled by the contact zone between the carbonate rock and the Yangxin rock body,which mainly occurs in the contact zone skarn and near-contact zone altered rock body.It is believed that the deposits are related to the Yanshanian quartz syenite diorite magmatism.The contact zone between the quartz syenite and carbonate rocks is an advantageous location for searching for copper polymetallic deposits.Skarnization and silicification are important signs for prospecting.The article believes that the copper polymetallic ore body found in the Yejiazhuang mining area still has the potential of further expansion,and it also has the possibility to explore porphyry copper deposits. |
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Keywords: | copper-polymetallic deposits Yangxin rock body geological characteristics prospecting direction Yejiazhuang |
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