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    铌钽铁矿U⁃Pb年代学方法研究进展

    涂家润 张妍 周红英 崔玉荣 李国占 吴磊 李志丹

    涂家润, 张妍, 周红英, 崔玉荣, 李国占, 吴磊, 李志丹, 2025. 铌钽铁矿U⁃Pb年代学方法研究进展. 地球科学, 50(7): 2498-2510. doi: 10.3799/dqkx.2025.091
    引用本文: 涂家润, 张妍, 周红英, 崔玉荣, 李国占, 吴磊, 李志丹, 2025. 铌钽铁矿U⁃Pb年代学方法研究进展. 地球科学, 50(7): 2498-2510. doi: 10.3799/dqkx.2025.091
    Tu Jiarun, Zhang Yan, Zhou Hongying, Cui Yurong, Li Guozhan, Wu Lei, Li Zhidan, 2025. Progress in U⁃Pb Dating Methods of Columbite⁃Tantalite Minerals. Earth Science, 50(7): 2498-2510. doi: 10.3799/dqkx.2025.091
    Citation: Tu Jiarun, Zhang Yan, Zhou Hongying, Cui Yurong, Li Guozhan, Wu Lei, Li Zhidan, 2025. Progress in U⁃Pb Dating Methods of Columbite⁃Tantalite Minerals. Earth Science, 50(7): 2498-2510. doi: 10.3799/dqkx.2025.091

    铌钽铁矿U⁃Pb年代学方法研究进展

    doi: 10.3799/dqkx.2025.091
    基金项目: 

    国家自然科学基金项目 42473029

    国家自然科学基金项目 42473031

    国家自然科学基金项目 42103025

    详细信息
      作者简介:

      涂家润(1986-),男,博士,高级工程师,主要从事同位素地质年代学和地球化学研究. ORCID:0009-0001-6443-3089. E-mail:jrtu@mail.nankai.edu.cn

      通讯作者:

      张妍, ORCID: 0009-0005-9052-0070. E-mail:zhangyannku@nankai.edu.cn

    • 中图分类号: P597

    Progress in U⁃Pb Dating Methods of Columbite⁃Tantalite Minerals

    • 摘要:

      铌钽铁矿具有高封闭温度、高铀含量及低普通铅特征,是开展U-Pb定年的理想矿物,其同位素年代学能为稀有金属花岗岩及花岗伟晶岩成因机制研究提供关键约束.铌钽铁矿U-Pb定年方法主要包括同位素稀释‒热电离质谱法(ID-TIMS)、激光剥蚀电感耦合等离子体质谱法(LA-ICP-MS)及二次离子质谱法(SIMS).系统梳理了三种定年方法的基本原理、发展脉络、技术优势及现存问题,并重点总结了近年来该方法在稀有金属矿床成矿时代厘定、成矿过程解析等领域的应用进展.由于铌钽铁矿端元成分复杂多变,且常用的微区原位测年方法(LA-ICP-MS/SIMS)普遍存在基体效应的影响,实现多期次成矿事件中铌钽铁矿U-Pb年龄的高精度、高准确度测定仍是当前技术难点及未来研究重点.

       

    • 图  1  铌钽铁矿JEQ-2 LA-MC-ICP-MS U-Pb定年结果

      a.采用铌铁矿标样coltan139作为校正外标;b.采用钽铁矿标样CT1作为校正外标(数据来源于Yang et al.,2024

      Fig.  1.  LA-MC-ICP-MS U-Pb dating results of columbite-tantalite JEQ-2

      图  2  文献中已报道的铌钽铁矿标样成分判别图解(据Qing et al.,2024修改

      Fig.  2.  Quadrilateral diagram of the reported columbite-tantalite reference materials (modified after Qing et al., 2024)

      表  1  文献中报道的铌钽铁矿标样统计

      Table  1.   Statistics of the columbite-tantalite reference materials from references

      标样
      名称
      主要元素平均含量(%) 比值 微量元素含量(10‒6 产地 ID-TIMS年龄(Ma) 参考文献
      FeO MnO Nb2O5 Ta2O5 Mn# Ta# U Pb 普通Pb
      Coltan139 14.14 6.45 62.58 12.67 0.47 0.11 1 350±227 103±15 变化 马达加斯加 505.4±1.0a Melcher et al., 2015
      506.6±2.4b Melcher et al., 2015
      507.9±1.3c Yang et al., 2023
      Buranga 10.63 0.83 64.40 11.59 0.48 0.10 80±15 12±4.1 变化 卢旺达 936±14a Dewaele et al., 2011
      905.2±3.2a Legros et al., 2019
      Rongi 14.14 6.45 65.68 10.96 0.32 0.09 81±23 16±13 变化 卢旺达 931.5±2.5a Melcher et al., 2015
      OXF 10.79 10.16 69.71 8.12 0.49 0.07 479±332 20±14 美国 262.85±0.61d Qing et al., 2024
      ZKW 5.88 12.67 50.80 29.95 0.69 0.27 205±168 6±5 变化 中国四川 203.0±1.6c Yang et al., 2023
      DDB 7.86 11.40 58.51 20.74 0.60 0.18 515±130 16±3.3 变化 中国四川 202.0±1.0c Yang et al., 2023
      SN3 17.35 2.53 65.45 10.38 0.13 0.09 585±249 36±17 中国山西 404.0±1.3c Xiang et al., 2023
      HND 11.30 8.27 60.88 18.53 0.43 0.15 357±139 7±3 变化 中国湖北 136.2±0.9c Xiang et al., 2023
      RL2 10.40 6.91 34.81 47.18 0.40 0.45 486±343 10±7 变化 中国湖南 135.7±0.3c Xiang et al., 2023
      NP2 10.50 6.54 42.70 38.10 0.38 0.51 257±67 15±3 中国福建 380.3±2.4a Legros et al., 2019
      CC1716 15.40 6.11 70.50 6.50 0.28 0.10 268±427 26±6 变化 法国 326.3±0.6a Legros et al., 2019
      A-1 2.87 14.30 27.70 54.60 0.83 0.70 215±309 12±9 中国新疆 198.3±1.4a Legros et al., 2019
      ISSIA2 6.46 9.72 18.40 63.30 0.60 0.80 503±552 137±350 科特迪瓦 2 002±32a Legros et al., 2019
      CT1 14.57 0.84 7.08 74.72 0.06 0.86 199±12 72±5 科特迪瓦 2 046.8±1.1a Legros et al., 2019
      CT3 14.35 0.94 6.25 75.46 0.06 0.88 308±16 112±7 科特迪瓦 2 053.2±1.3a Legros et al., 2019
      CT4 14.80 0.62 7.51 75.10 0.04 0.92 176±8 65±4 变化 科特迪瓦 2 044±1.6a Legros et al., 2019
      注:(1)Mn♯=Mn/(Fe+Mn),Ta♯=Ta/(Nb+Ta).(2)ID-TIMS U-Pb年龄检测实验室所在机构,a为Bundesanstalt für Geowissenschaften und Rohstoffe(BGR),b为University of Toronto,c为German Research Centre for Geosciences(GFZ),d为中国地质调查局天津地质调查中心(Tianjin Center,China Geological Survey).
      下载: 导出CSV
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    • 收稿日期:  2025-03-31
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