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    榴辉岩中金红石的矿物地球化学研究及其意义

    陈振宇 王登红 陈毓川 徐珏 余金杰 王平安

    陈振宇, 王登红, 陈毓川, 徐珏, 余金杰, 王平安, 2006. 榴辉岩中金红石的矿物地球化学研究及其意义. 地球科学, 31(4): 533-538.
    引用本文: 陈振宇, 王登红, 陈毓川, 徐珏, 余金杰, 王平安, 2006. 榴辉岩中金红石的矿物地球化学研究及其意义. 地球科学, 31(4): 533-538.
    CHEN Zhen-yu, WANG Deng-hong, CHEN Yu-chuan, XU Jue, YU Jin-jie, WANG Ping-an, 2006. Mineral Geochemistry of Rutile in Eclogite and Its Implications. Earth Science, 31(4): 533-538.
    Citation: CHEN Zhen-yu, WANG Deng-hong, CHEN Yu-chuan, XU Jue, YU Jin-jie, WANG Ping-an, 2006. Mineral Geochemistry of Rutile in Eclogite and Its Implications. Earth Science, 31(4): 533-538.

    榴辉岩中金红石的矿物地球化学研究及其意义

    基金项目: 

    国家重点基础研究发展规划项目 2003CB716507

    详细信息
      作者简介:

      陈振宇(1978-), 男, 助研, 在读博士研究生, 主要从事矿物地球化学和微束分析研究.E-mail: czy7803@126.com

    • 中图分类号: P578.4

    Mineral Geochemistry of Rutile in Eclogite and Its Implications

    • 摘要: 金红石的微量元素分析在俯冲带地质作用示踪、榴辉岩原岩判别以及形成温度估算等的研究中具有重要指示作用, 其U-Pb同位素和Hf同位素分析则对于确定高级变质岩的冷却时代以及探讨物质来源和壳幔作用过程具有重要意义.初步研究显示, 苏鲁超高压变质地体及大陆科学钻探岩心中不同产状、不同类型的榴辉岩中的金红石具有不同的微量元素特征, 对榴辉岩原岩及金红石形成温度具有很好的指示作用; 3个金红石样品的Pb同位素组成在逐步淋溶分析的某个中间阶段和最后阶段均出现有相似规律的2次突变, 其余阶段则相对平稳, 有可能反映了金红石在其生长过程中构造环境背景的变化.进一步对金红石进行详细系统的矿物地球化学分析, 有望在苏鲁地体大陆深俯冲-折返过程的地球动力学及榴辉岩型金红石矿床的研究中获得一些新的认识.

       

    • 图  1  金红石的铅同位素组成图解

      Fig.  1.  Plot of Pb isotope composition of rutiles

      图  2  金红石在逐步淋溶过程中铅同位素组成的变化

      Fig.  2.  Variation of Pb isotope composition of rutile during step leaching

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    • 收稿日期:  2006-04-05
    • 刊出日期:  2006-07-25

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