| 福建永定新村钼铅锌多金属矿床地质特征及成因探讨 |
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| 引用本文： | 韩胜康.福建永定新村钼铅锌多金属矿床地质特征及成因探讨[J].福建地质,2008,27(4):352-360. |
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| 作者姓名： | 韩胜康 |
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| 作者单位： | 福建省地质调查研究院,福州,350003 |
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| 摘 要： | 永定新村钼铅锌多金属矿床位于闽西南断陷带和闽东火山断坳带结合处，属武夷山成矿带。地表以近东西向、北东向构造控制的细脉浸染型钼铅锌矿化为主，磁异常、电异常、土壤地化异常套合好，浓集中心明显。经过综合资料分析，表明永定新村钼铅锌矿床成因类型属岩浆热液充填交代型矿床。
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| 关 键 词： | 钼铅锌矿床 火山断坳带 岩浆热液充填交代型 武夷山成矿带 福建永定 |
On the Geologic Characteristics and Genesis of the Xincun Molybdenum, Led and Zinc Polymetallic Deposit in Yongding County, Fujian Province |
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| Han Shengkang.On the Geologic Characteristics and Genesis of the Xincun Molybdenum, Led and Zinc Polymetallic Deposit in Yongding County, Fujian Province[J].Geology of Fujian,2008,27(4):352-360. |
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| Authors: | Han Shengkang |
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| Institution: | Han Shengkang ( Fujian Institute of Geological Survey and Research, Fuzhou , 350003 ) |
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| Abstract: | The Xincun molybdenum, led and zinc polymetallic deposit is situated at the juncture of the Southwest Fujian rift depression zone and the East Fujian volcanic fault sag zone, which belongs to the Wuyishan metallogenetic belt. On the earth's surface, it gives priority to the veinlet and impregnating type of molybdenum lead-zinc metallization controlled by the near east-west and east-northeast structures. The magnetic anomaly, electrical anomaly and soil geochemical anomalies have a better telescoping and the contraction center of the anomalies is obvious. Based on the analyses of the integrated geological data, it is considered that the Xincun molybdenum lead-zinc deposit in Yongding County belongs to the mineral deposit of the magmatic hydrothermal filling and metasomatic type. |
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| Keywords: | molybdenum lead and zinc deposit volcanic fault sag zone magmatic hydrothermal filling and metasomatic type Wuyishan metallogenetic belt Yongding County Fujian Province |
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