| 福建顺昌小王历铅锌多金属矿床地质特征及成因探讨 |
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| 引用本文： | 潘飞.福建顺昌小王历铅锌多金属矿床地质特征及成因探讨[J].福建地质,2012,31(3):215-223. |
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| 作者姓名： | 潘飞 |
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| 作者单位： | 福建省闽北地质大队,福州,350000 |
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| 摘 要： | 顺昌小王历铅锌矿体主要产于中-晚元古代变质岩基底内的构造破碎带内,矿体呈长脉状,透镜状或似层状,分布于南北向及北北东向构造破碎带内,为中低温热液充填交代矿床,达到中型规模。
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| 关 键 词： | 铅锌矿 地质特征 矿床成因 岩浆热液 顺昌小王历 |
On the Geologic Characteristics and Genesis of the Xiaowangli Polymetallic Deposit in Shunchang County, Fujian Pro. |
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| Pan Fei.On the Geologic Characteristics and Genesis of the Xiaowangli Polymetallic Deposit in Shunchang County, Fujian Pro.[J].Geology of Fujian,2012,31(3):215-223. |
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| Authors: | Pan Fei |
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| Institution: | Pan Fei (Northern Fujian Geologic Party of Fujian Province, Shaowu, 354000) |
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| Abstract: | The Xiaowangli lead -zinc deposit mainly exist in the tectonic fracture zone of middle and late Proterozoic metamporphic basement. The orebodies act like the veiny, lenticular and parabedded forms and are distributed over the NS and NNE tectonic fracture zone. The deposit with mid-scale belongs to the mineral deposit of the medium-low hydrothermal filling and metasomatic type. |
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| Keywords: | lead and zinc deposit geologic characteristics genesis of mineral deposit magmatic hydrotherm Xiaowangli deposit of Shunchang County |
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