| 闽西北常口—南舟断裂带与萤石成矿关系 |
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| 引用本文： | 傅树超,苏江湖.闽西北常口—南舟断裂带与萤石成矿关系[J].福建地质,1997,16(4):170-175. |
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| 作者姓名： | 傅树超 苏江湖 |
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| 作者单位： | 福建省区域地质调查队!三明，365001，福建省区域地质调查队!三明，365001，福建省区域地质调查队!三明，365001 |
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| 摘 要： | 福建省区域地质调查队三分队在元坑幅及埔上幅１：５万区调中分别发现了将乐常口大型萤石矿和顺昌南舟萤石矿。两个矿床均位于常口－南舟北东向断裂带中，受其次级张性断裂直接控制，矿床成因类似。
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| 关 键 词： | 断裂带 萤石 矿化 硅化 矿床成矿 |
On Mineralizational Relations of the Changkou and Nanzhou Fluorite Deposits with the Changkou-Nanzhou Fault Belt in Northwestern Fujian |
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| Fu Shuchao, Su Jianghu , Huang Zhonglin.On Mineralizational Relations of the Changkou and Nanzhou Fluorite Deposits with the Changkou-Nanzhou Fault Belt in Northwestern Fujian[J].Geology of Fujian,1997,16(4):170-175. |
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| Authors: | Fu Shuchao Su Jianghu Huang Zhonglin |
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| Abstract: | The Changkou and Nanzhou fluorite deposits, located in Jiangle and Shunchang countiesof Northwestern Fujian and dlscovered in 1984 and 1996, were suitated in the ChangkouNanzhou NE-trend Fault Belt and controlled directly by its secondary extension faults. Afteranalyzing the ore-forming conditions of both deposits,it is indicated that both deposits belongto a same genetic type and the area along the Changkou - Nanzhou Fault Belt is a goodprospective ore-forming province. |
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| Keywords: | fault belt fluorite mineralization silicification Northwestern Fujian |
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