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福建大坪花岗斑岩型稀有金属矿床铌铁矿LA-ICP-MS U-Pb定年及其地质意义
LA-ICP-MS U-Pb Age of Columbite from the Daping Granite Porphyry-type Rare Metal Deposit in Fujian Province and Its Geological Significance

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王锦荣 1,2   吕正航 3   吕新彪 1 *   林培军 4  
文摘 最近在福建永定大坪发现了特大型花岗斑岩型钽铌矿,为确定该矿床的成矿年龄和类型,利用LA-ICP-MS对该矿的铌铁矿进行了U-Pb年代学研究。结果显示,大坪铌铁矿的成矿年龄为183 Ma左右,该年龄与成岩年龄在误差范围内一致,表明华南地区存在早侏罗世花岗斑岩型钽铌成矿事件。大坪早侏罗世花岗斑岩型钽铌矿成矿时间和类型是对华南钽铌成矿研究的重要补充,为华南未来的钽铌找矿方向提供了新的思路。
其他语种文摘 In this work,the U-Pb chronology of columbite-tantalite group minerals (CGM) from the Daping super-large granite porphyry-type Ta-Nb ore deposit,which was recently discovered,in Yongding County,Fujian Province,have been conducted,in order to constrain mineralization age and type of the deposit. The results show that the mineralization age of the Daping Nb-Ta ore deposit is ca. 183 Ma which is consistent with the age of granite porphyry within analytical deviation, indicating that there is an Early Jurassic granite porphyry-type Ta-Nb mineralization event in South China. Therefore, it is believed that the discovery of the Daping Early Jurassic granite porphyry-type Ta-Nb ore deposit has provided an important supplement,in terms of mineralization time and metallogenic type,for studying the Nb-Ta mineralization in South China,and an new clue for prospecting Ta-Nb mineral resource in South China in future.
来源 矿物岩石地球化学通报 ,2020,39(3):637-645 【核心库】
DOI 10.19658/j.issn.1007-2802.2020.39.020
关键词 U-Pb年代学 ; 铌铁矿 ; 稀有金属 ; 花岗斑岩 ; 福建
地址

1. 中国地质大学(武汉)资源学院, 武汉, 430074  

2. 中国冶金地质总局第二地质勘查院, 福州, 350108  

3. 中国科学院地球化学研究所, 中国科学院地球内部物质与高温高压院重点实验室, 贵阳, 550081  

4. 中国冶金地质总局山东局测试中心, 济南, 250014

语种 中文
文献类型 研究性论文
ISSN 1007-2802
学科 地质学
基金 科技部重点研发计划项目 ;  国土资源部中国地质调查局地质调查项目
文献收藏号 CSCD:6750513

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引证文献 2

1 郭春丽 中国花岗岩型锂矿床:重要特征、成矿条件及形成机制 岩石学报,2024,40(2):347-403
被引 1

2 季浩 碱性花岗岩型稀有稀土矿床类型及成矿作用研究进展 地质科技通报,2024,43(1):23-38
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