闽北羊角尾萤石矿成因:来自稀土、微量元素地球化学的证据

金松, 王春连, 高立湧, 张成信, 王占兵, 王畅, 孟都, 商朋强. 2022. 闽北羊角尾萤石矿成因:来自稀土、微量元素地球化学的证据[J]. 地球学报, 43(3): 371-382. doi: 10.3975/cagsb.2022.031401
引用本文: 金松, 王春连, 高立湧, 张成信, 王占兵, 王畅, 孟都, 商朋强. 2022. 闽北羊角尾萤石矿成因:来自稀土、微量元素地球化学的证据[J]. 地球学报, 43(3): 371-382. doi: 10.3975/cagsb.2022.031401
JIN Song, WANG Chun-lian, GAO Li-yong, ZHANG Cheng-xin, WANG Zhan-bing, WANG Chang, MENG Du, SHANG Peng-qiang. 2022. Evidence from REE and Trace Element Geochemistry for Genesis of Yangjiaowei Fluorite Deposit in Northern Fujian. Acta Geoscientica Sinica, 43(3): 371-382. doi: 10.3975/cagsb.2022.031401
Citation: JIN Song, WANG Chun-lian, GAO Li-yong, ZHANG Cheng-xin, WANG Zhan-bing, WANG Chang, MENG Du, SHANG Peng-qiang. 2022. Evidence from REE and Trace Element Geochemistry for Genesis of Yangjiaowei Fluorite Deposit in Northern Fujian. Acta Geoscientica Sinica, 43(3): 371-382. doi: 10.3975/cagsb.2022.031401

闽北羊角尾萤石矿成因:来自稀土、微量元素地球化学的证据

  • 基金项目:

    本文由中国地质调查局地质调查项目(编号: DD20190816

    DD20190606)、中化地质矿山总局化工地质科技项目(编号: ZHDK202004)和中央级公益性科研院所基本科研业务费专项(编号: KK2005)联合资助

详细信息
    作者简介: 金松, 男, 1988年生。硕士, 工程师。主要从事区域矿产地质调查工作。E-mail: 732818885@qq.com
    通讯作者: 王春连, 男, 1983年生。博士, 研究员。主要从事矿床学方面的研究。通讯地址: 100037, 北京市西城区百万庄大街26号。E-mail: wangchunlian312@163.com
  • 中图分类号: P611.1; P619.215

Evidence from REE and Trace Element Geochemistry for Genesis of Yangjiaowei Fluorite Deposit in Northern Fujian

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    Corresponding author: WANG Chun-lian
  • 闽北浦城羊角尾萤石矿产于侏罗系梨山组火山碎屑岩中的断裂破碎带内, 对其地质矿产特征和矿石、围岩及矿区内黑云母正长花岗岩的岩石地球化学特征进行了研究。羊角尾萤石矿矿石∑REE为65.17×10–6~125.87×10–6, 重稀土相对富集, δEu 和 δCe无明显异常; Ni、Cd、Pb 和 As等中低温微量元素相对地壳富集。围岩梨山组火山碎屑岩轻重稀土分馏不明显, Eu负异常明显, Sm/Nd值与萤石接近, 微量元素相对地壳的含量曲线趋势与萤石基本一致。黑云母正长花岗岩则显示轻稀土富集、重稀土亏损, Eu正异常和Ce负异常的特征, Sm/Nd值远小于萤石矿。结合稀土微量元素特征及矿床成因判别图解, 认为羊角尾萤石矿的主要成矿物质来源为梨山组火山碎屑岩。成矿流体在形成后经历了长期的演化, 在此过程中与围岩发生了充分的水岩反映, 使Ca、F、REE等重新活化, 最终在构造破碎带就位沉淀形成矿体, 矿床成因类型为中-低温热液充填型。羊角尾萤石矿的矿床成因研究表明晚侏罗世火山-沉积岩系是区域萤石矿成矿的重要物源基础, 在区域找矿工作中应重点关注。
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