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    “孪生元素”铌-钽的地球化学特性和研究进展

    谭东波 李东永 肖益林

    谭东波, 李东永, 肖益林, 2018. “孪生元素”铌-钽的地球化学特性和研究进展. 地球科学, 43(1): 317-332. doi: 10.3799/dqkx.2018.019
    引用本文: 谭东波, 李东永, 肖益林, 2018. “孪生元素”铌-钽的地球化学特性和研究进展. 地球科学, 43(1): 317-332. doi: 10.3799/dqkx.2018.019
    Tan Dongbo, Li Dongyong, Xiao Yilin, 2018. Geochemical Characteristics of Niobium and Tantalum: A Review of Twin Elements. Earth Science, 43(1): 317-332. doi: 10.3799/dqkx.2018.019
    Citation: Tan Dongbo, Li Dongyong, Xiao Yilin, 2018. Geochemical Characteristics of Niobium and Tantalum: A Review of Twin Elements. Earth Science, 43(1): 317-332. doi: 10.3799/dqkx.2018.019

    “孪生元素”铌-钽的地球化学特性和研究进展

    doi: 10.3799/dqkx.2018.019
    基金项目: 

    国家自然科学基金项目 41473033

    国家自然科学基金项目 41673031

    详细信息
      作者简介:

      谭东波(1992-), 男, 博士研究生, 主要从事元素地球化学和同位素地球化学研究

      通讯作者:

      肖益林

    • 中图分类号: P588

    Geochemical Characteristics of Niobium and Tantalum: A Review of Twin Elements

    • 摘要: 因为具有相同的离子电价(+5)及相似的离子半径(~0.064 nm),铌和钽是地球化学性质非常相似的一对"孪生"元素.作为高场强元素,Nb-Ta通常赋存在金红石、角闪石、铌-钽矿、榍石和云母等矿物中.近20年来特别是21世纪初,Nb、Ta一直是地球化学领域的一个热点,大量的研究关注不同铌-钽矿物的赋存状态、矿物和岩石中铌-钽含量和铌/钽比值、铌-钽矿物与熔/流体之间的元素分配的实验岩石学研究和铌-钽分异的机制及具体地质过程.研究Nb、Ta具有重要的科学意义,涉及到整个地球的元素平衡、大陆地壳的生长机制、含金红石岩石的形成源区等.本文综合了近20年来铌、钽的研究内容,系统地总结了铌、钽在地球化学研究中各方面已经取得的成果,同时展望了未来铌-钽这对高场强元素对在地球科学研究中的潜在应用.

       

    • 图  1  太阳系中不同岩石类型的Nb/Ta比值

      数据据Jochum et al.(1986)Barth et al.(2000)Rudnick et al.(2000)Kamber and Collerson(2000)Münker et al.(2003)Münker et al.(2004)Workman and Hart(2005)Pfänder et al.(2007).黑色五角星代表各类岩石的平均Nb/Ta比值

      Fig.  1.  Nb/Ta ratios of different types of rocks in the solar system

      图  2  硅酸盐地球不同地质储库的Nb-Nb/Ta关系

      数据来源:Chondrite据Münker et al.(2003);DM据Rudnick et al.(2000)Workman and Hart(2005);UCC据Barth et al.(2000);IAB据Münker et al.(2004);HIMU、EM1和EM2据Pfänder et al.(2007)

      Fig.  2.  The Nb content and Nb/Ta ration diagram of main geological reservoirs in the Earth

      图  3  平均弧玄武岩和板片内产生的岩浆的混合曲线

      图改自Barth et al.(2000);Average arc basalt的数据来自于Mcculloch amd Gamble(1991);板片内产生的岩浆的数据来自于Sun and McDonough(1989)Neal et al.(1997)

      Fig.  3.  Mixing relationships between average arc basalt and intraplate magmas

      图  4  不同变质岩性中金红石Nb-Cr判别图解

      a.改自Zack et al.(2004a),注意长英质片麻岩中的Nb含量可达28 500×10-6;b.改自Triebold et al.(2007),当lg(Cr/Nb)>0时,说明金红石来自于变镁铁质岩石,反之,来自于变泥质岩;c.改自Meinhold et al.(2008),注意变泥质岩中金红石的Nb含量下限为800×10-6

      Fig.  4.  Rutile Nb-Cr discrimination diagram in different metamorphic lithology

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