| 福建政和湖屯铅锌矿地质特征及找矿远景浅析 |
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| 引用本文： | 张文瑞.福建政和湖屯铅锌矿地质特征及找矿远景浅析[J].福建地质,2009,28(3):181-187. |
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| 作者姓名： | 张文瑞 |
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| 作者单位： | 中国地质大学,武汉,430047;福建省闽北地质大队,福州,350002 |
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| 摘 要： | 湖屯铅锌矿主要产于中-晚元古代变质岩基底与火山岩接触部位或“天窗”内外，矿体呈脉状、透镜状、似层状，受变质岩层位与后期断裂构造控制，矿床成因类型为海底火山喷发-沉积变质（热液改造）块状硫化物型和构造蚀变岩型硫化物矿床。区内异常范围大，浓度高，成矿条件好。
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| 关 键 词： | 铅锌矿 地质特征 找矿远景 政和湖屯 |
On the Geologic Characteristics and Ore-finding Perspective of the Hutun Lead-zinc Ores in Zhenghe County,Fujian Province |
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| Zhang Wenrui.On the Geologic Characteristics and Ore-finding Perspective of the Hutun Lead-zinc Ores in Zhenghe County,Fujian Province[J].Geology of Fujian,2009,28(3):181-187. |
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| Authors: | Zhang Wenrui |
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| Institution: | Zhang Wenrui(Northern Fujian Geologic Party of Fujian Province,Fuzhou,350002) |
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| Abstract: | The Hutun lead-zinc ores exist mainly in the contact site between the middle and late Proterozoic metamorphic basement and volcanic rocks or in the internal and external sky-light window.The orebodies act like the veiny,lenticular and parabedded forms and are controlled by the stratigraphic position of metamorphic rocks and the faulted structures of late stage.In the genetic type of the mineral deposit,it belongs to sulfide mineral deposit of the submarine volcano eruption and diagenetic metamorphism(hydrot... |
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| Keywords: | lead-zinc ores geologic characteristics ore-finding perspective Zhenghe County |
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