| 江西黎川岭下金多金属矿床地质特征及找矿标志 |
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| 引用本文： | 张进高.江西黎川岭下金多金属矿床地质特征及找矿标志[J].福建地质,2014,33(4):271-277. |
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| 作者姓名： | 张进高 |
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| 作者单位： | 福建省地质测绘院,福州,350011 |
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| 摘 要： | 黎川岭下金多金属矿处于武夷山成矿带中部,闽西北隆起带西缘,区内经长期强烈的构造叠加活动,导致岩浆侵入上升,构造和岩浆活动提供的大量含矿热流体沿断裂贯入、迁移,从而富集成矿.矿体呈脉状、线脉状、透镜体状贮存于北东东向构造带中,为构造热液蚀变型矿床.
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| 关 键 词： | 金多金属矿 地质特征 找矿标志 黎川岭下 |
Geological Characteristics and Prospecting Marks of Lingxia Gold Polymetallic Deposit in Lichuan County,Jiangxi Province |
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| Zhang Jingao.Geological Characteristics and Prospecting Marks of Lingxia Gold Polymetallic Deposit in Lichuan County,Jiangxi Province[J].Geology of Fujian,2014,33(4):271-277. |
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| Authors: | Zhang Jingao |
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| Institution: | Zhang Jingao (Fujian Institute of Geological Survey and Drawing, Fuzhou, 350011) |
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| Abstract: | Lingxia gold polymetallic deposit is in central Wuyishan metallogenic belt and in western uplift of northwestern Fujian province. Long term strong structural overprinting activity lead to magma intrusion rising in the region. The large ore-bearing metallogenetic fluids inject and move along the fractured zones by tectonic and magmatic activity, which leads to the gold concentration and mineralization. Ore bodies are veins, thread veins and lens-shaped . They are stored in the Nee tectonic belt. It belongs to the tectonic hydrothermal alteration deposit. |
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| Keywords: | gold polymetallic deposits metallogenic geological characteristics prospecting mark Lingxia of Lichuan county |
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