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    华北克拉通东部及苏鲁造山带的地壳生长: 来自现代河流碎屑锆石的U-Pb定年和Hf同位素证据

    耿显雷 高山 陈晨

    耿显雷, 高山, 陈晨, 2011. 华北克拉通东部及苏鲁造山带的地壳生长: 来自现代河流碎屑锆石的U-Pb定年和Hf同位素证据. 地球科学, 36(3): 483-499. doi: 10.3799/dqkx.2011.050
    引用本文: 耿显雷, 高山, 陈晨, 2011. 华北克拉通东部及苏鲁造山带的地壳生长: 来自现代河流碎屑锆石的U-Pb定年和Hf同位素证据. 地球科学, 36(3): 483-499. doi: 10.3799/dqkx.2011.050
    GENG Xian-lei, GAO Shan, CHEN Chen, 2011. Crustal Growth of the Eastern North China Craton and Sulu Orogen as Revealed by U-Pb Dating and Hf Isotopes of Detrital Zircons from Modern Rivers. Earth Science, 36(3): 483-499. doi: 10.3799/dqkx.2011.050
    Citation: GENG Xian-lei, GAO Shan, CHEN Chen, 2011. Crustal Growth of the Eastern North China Craton and Sulu Orogen as Revealed by U-Pb Dating and Hf Isotopes of Detrital Zircons from Modern Rivers. Earth Science, 36(3): 483-499. doi: 10.3799/dqkx.2011.050

    华北克拉通东部及苏鲁造山带的地壳生长: 来自现代河流碎屑锆石的U-Pb定年和Hf同位素证据

    doi: 10.3799/dqkx.2011.050
    基金项目: 

    国家自然科学基金 40973020

    国家自然科学基金 0714010

    国家自然科学基金 0821061

    教育部高等学校学科创新引智计划 B07039

    霍英东教育基金 121017

    详细信息
      作者简介:

      耿显雷(1986-), 男, 硕士研究生, 主要从事岩石圈地球化学的研究

      通讯作者:

      高山, sgao@263.net

    • 中图分类号: P597

    Crustal Growth of the Eastern North China Craton and Sulu Orogen as Revealed by U-Pb Dating and Hf Isotopes of Detrital Zircons from Modern Rivers

    • 摘要: 来自年轻沉积物或现代河流的碎屑锆石是研究大陆地壳生长演化的理想载体.为揭示华北克拉通东部和苏鲁造山带大陆地壳的生长演化, 采集了中国东部大清河、潮白河、辽河、大沽河和胶莱河的5个地方的河沙样品, 并对分选出来的碎屑锆石进行了LA-ICP-MS和MC-LA-ICP-MS U-Pb定年和Hf同位素微区原位分析, 获得了396个锆石U-Pb谐和年龄及其对应的Hf同位素组成.2.4~2.5 Ga和1.8~1.9 Ga两个年龄特征峰指示大清河、潮白河和辽河的碎屑锆石来源于华北克拉通东部.辽河一部分100~500 Ma的锆石具有正的εHf(t)值和年轻的Hf模式年龄, 显示出显生宙的地壳生长.苏鲁造山带大沽河和胶莱河的碎屑锆石U-Pb年龄分布相对比较复杂, 但锆石U-Pb年龄和Hf同位素特征表明其为华北克拉通和扬子克拉通的混合来源.来自大清河、潮白河和辽河的锆石U-Pb年龄和Hf同位素证据, 表明华北克拉通东部地壳生长的主要时期为2.4~3.0 Ga, 并在2.6~2.7 Ga时处于生长的最高峰, 次一级的生长期为1.3~2.3 Ga, 而在其他阶段几乎没有地壳的生长或者不明显.华北克拉通东部现存大陆地壳的80%来源于太古代和古元古代的生长, 而自古元古代开始大陆地壳的演化就以古老地壳的重熔再改造为主.此外, 大沽河碎屑锆石的Hf同位素组成揭示出苏鲁造山带在古生代(300~500 Ma)存在明显的地壳生长.

       

    • 图  1  中国东部主要构造简图(a)及河流采样图(b)

      EB.华北克拉通东部块体,TNCO.华北克拉通中部造山带;WB.华北克拉通西部块体,YC.扬子克拉通,SC.华南造山带

      Fig.  1.  Simplified map of major tectonic units in China (a) and the drainage area of the Daqing River, Chaobai River, Liao River, Dagu River and Jiaolai River under this investigation and sample location (b)

      图  2  锆石U-Pb谐和图(a)和U-Pb年龄频谱图(b)

      Fig.  2.  2U-Pb concordia plots of concordant detrital zircons (a) and corresponding relative probability plots of U-Pb ages for concordant detrital zircons (b)

      图  3  谐和锆石的U-Pb年龄-εHf(t)

      Fig.  3.  U-Pb age versus εHf(t) value plots of concordant detrital zircons

      图  4  谐和锆石的U-Pb年龄-Th/U分布

      Fig.  4.  Plots of Th/U ratios versus U-Pb ages of concordant detrital zircons

      图  5  华北克拉通和扬子克拉通的年龄特征对比

      华北克拉通的数据来自文献Zhao et al.(2001)Gao et al.(2004)及其所引文献,扬子克拉通的数据来自文献Liu et al.(2008)

      Fig.  5.  Comparison of zircon U-Pb age distributions of Yangtze craton and North China craton

      图  6  潮白河、辽河、大清河、大沽河和胶莱河不同年龄组锆石的TDM2(Hf)分布

      Fig.  6.  Corresponding relative probability plots of TDM2 (Hf) for different age group zircons

      图  7  辽河及中亚造山带东部显生宙锆石的TDM2(Hf)分布对比(中亚造山带东部的数据来自文献程瑞玉等, 2006; Chen et al., 2009; Meng et al., 2010)

      Fig.  7.  Comparison of two-stage Hf crust formation model ages of Phanerozoic zircons for the Liao River and eastern of the eastern Central Asian orogenic belt (CAOB)

      图  8  潮白河、辽河和大清河谐和锆石累计的U-Pb年龄及TDM2(Hf)分布>

      Fig.  8.  Corresponding relative probability plots of TDM2(Hf) for zircons from the Chaobai River, Liao River and Daqing River

      图  9  TDM2(Hf)指示的华北克拉通东部地壳生长速率

      Fig.  9.  Crust growth rate of the eastern North China Craton indicated by TDM2 (Hf)

      图  10  华北克拉通东部基于大清河、潮白河和辽河碎屑锆石U-Pb年龄和TDM2(Hf)的累计生长曲线

      Fig.  10.  Crust growth curves of the eastern North China craton based on U-Pb ages and two-stage Hf crust formation ages for detrital zircons from the Daqing River, Chaobai River and Liao River

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