| 周宁芹溪铅锌银矿床地质特征与成因初探 |
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| 引用本文： | 周辉能.周宁芹溪铅锌银矿床地质特征与成因初探[J].福建地质,2005,24(1):19-24. |
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| 作者姓名： | 周辉能 |
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| 作者单位： | 福建省第四地质大队,宁德,352100 |
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| 摘 要： | 位于周宁芹溪铅锌银矿床产在晚侏罗—早白垩世中一酸性火山活动带上，成矿与断裂构造及次火山活动有关。该矿床经普查—详查工作，已基本查明了⑥号构造蚀变带矿床地质特征、控矿条件、矿体规模及形态特征，初步研究认为该矿床应属中低温浅成火山热液成因的硫化铅锌银矿。
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| 关 键 词： | 铅锌银矿 地质特征 中低温浅成火山热液 周宁芹溪 |
| 修稿时间： | 2004年7月13日 |
On Geologic Characteristics and Genesis of the Qinxi Lead-Zinc-Silver Deposit in Zhouning County |
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| Zhou Huineng.On Geologic Characteristics and Genesis of the Qinxi Lead-Zinc-Silver Deposit in Zhouning County[J].Geology of Fujian,2005,24(1):19-24. |
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| Authors: | Zhou Huineng |
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| Abstract: | The Qinxi lead-zinc-silver deposit in Zhouning County is discovered in the Late Jurassic to Early Cretaceous intermediate-acidic volcanic belt and the ore-forming process of the deposit is relative to the faulted structures and subvolcanic activity. The reconnaissance and detailed survey of the deposit has made certain of the ore-deposit geologic characteristics, the ore-control conditions, the orebody size and morphological characteristics in the No.6 structural altered zone. Based on the preliminary study, it is inferred that the deposit belongs to sulfureted lead-zinc-silver deposit derived from the low-to-moderate temperature hypabyssal volcanic-hydrothermal fluid. |
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| Keywords: | the lead-zinc-silver deposit geologic characteristics low-to-moderate temperature hypabyssal volcanic-hydrothermal fluid Zhouning County |
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