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    大别造山带中元古代变沉积岩碎屑锆石U-Pb年代学与Hf同位素特征及其地质意义

    孔令耀 郭盼 万俊 刘成新 王晶 陈超

    孔令耀, 郭盼, 万俊, 刘成新, 王晶, 陈超, 2022. 大别造山带中元古代变沉积岩碎屑锆石U-Pb年代学与Hf同位素特征及其地质意义. 地球科学, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096
    引用本文: 孔令耀, 郭盼, 万俊, 刘成新, 王晶, 陈超, 2022. 大别造山带中元古代变沉积岩碎屑锆石U-Pb年代学与Hf同位素特征及其地质意义. 地球科学, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096
    Kong Lingyao, Guo Pan, Wan Jun, Liu Chengxin, Wang Jing, Chen Chao, 2022. Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance. Earth Science, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096
    Citation: Kong Lingyao, Guo Pan, Wan Jun, Liu Chengxin, Wang Jing, Chen Chao, 2022. Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance. Earth Science, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096

    大别造山带中元古代变沉积岩碎屑锆石U-Pb年代学与Hf同位素特征及其地质意义

    doi: 10.3799/dqkx.2021.096
    基金项目: 

    中国地质调查局项目 DD20190050

    中国地质调查局项目 DD20190370

    湖北省地质局项目 KJ2020-65

    湖北省地质局项目 KJ2021-4

    详细信息
      作者简介:

      孔令耀(1989-),男,硕士,工程师,主要从事区域地质调查和造山带地层方面工作. ORCID:0000-0003-3759-7384. E-mial:951121661@qq.com

    • 中图分类号: P597

    Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance

    • 摘要: 大别造山带位于扬子陆块北缘,近年来的研究显示其发育太古代-古元古代的结晶基底,但一直缺乏中元古代的物质信息.首次报道了大别造山带核部一套中元古代“变砂岩-大理岩”变沉积岩组合,通过对该套地层的3个样品碎屑锆石U-Pb年代学和Lu-Hf同位素特征分析,显示最年轻的锆石平均年龄分别为:1 556±13 Ma、1 541±20 Ma和1 584.3±24 Ma,在误差范围内基本一致,说明该套地层的形成时代为中元古代,锆石变质增生边记录该套地层经历了124.1±2.3 Ma的变质事件,碎屑锆石年龄频谱和Lu-Hf同位素特征显示该套地层物源特征与神农架群一致;碎屑锆石峰值年龄2 682 Ma,2 461 Ma记录了“大别陆块”结晶基底两期重要生长事件,峰值年龄2 043 Ma,1 803 Ma和1 572 Ma显示“大别地块”可能参与Columbia超大陆聚合-裂解事件,在新元古代早期与“黄陵陆核”拼合而成为扬子陆块统一基底的重要组成部分.

       

    • 图  1  大别造山带区域地质简图及采样点

      Wu et al.(2008)邱啸飞等(2020)郭盼等(2021)修改

      Fig.  1.  Sketch geological map for the Dabie orogen and sampling location

      图  2  大别造山带中元古代变沉积岩典型地质剖面图

      Fig.  2.  Typical geological profile of Mesoproterozoic metasedimentary rocks in the Dabie orogen

      图  3  样品野外与镜下特征

      a. D2247-2条带状角闪石辉石石英岩呈“夹层”状产出在大理岩之中;b. D2247-2条带状角闪石辉石石英岩镜下特征(正交镜);c,d. PM209-22-2含二长辉石石英岩野外和镜下特征(正交镜);e,f. PM205-40-1含矽线二云钾长片麻岩野外和镜下特征(单偏光镜);Hbl.角闪石;Px.辉石;Qtz.石英;Pl.斜长石;Kf.钾长石;Sil.矽线石;Bi.黑云母;Ms.白云母

      Fig.  3.  Field outcrops and photomicrographs of samples

      图  4  样品D2247-2、PM209-22-2和PM205-40-1不同年龄锆石代表性CL图像特征

      白色实线圈为U-Pb测试点,黄色虚线圈为Lu-Hf测试点

      Fig.  4.  Typical CL images of different ages from the samples of D2247-2, PM209-22-2 and PM205-40-1

      图  5  锆石U-Pb年龄谐和图、频率直方图和平均年龄图

      Fig.  5.  The U-Pb concordia diagrams, frequency histograms and mean age diagrams

      图  6  样品D247-2碎屑锆石U-Pb年龄与εHf(t)关系(神农架群数据肖志斌,2012

      Fig.  6.  U-Pb age versus εHf(t) of detrital zircons from sample of D22247-2(after Xiao, 2012)

      图  7  分类回归树图和“变砂岩-大理岩”组合中碎屑锆石的原岩分类回归结果(Belousova et al. 2002

      Fig.  7.  Classification and regression tree(CART-tree) and source rock types of detrital zircons from the "metasandstone-marble"(after Belousova et al. 2002)

      图  8  “变砂岩-大理岩”组合中不同峰值年龄碎屑锆石U/Yb-Hf和U/Yb-Y图解(Grimes et al., 2007

      Fig.  8.  Plots of U/Yb-Hf and U/Yb-Y for different peak ages of detrital zircons from the "metasandstone-marble"

      图  9  大别地区中元古代“变砂岩-大理岩”组合与神农架群、扬子陆块碎屑锆石频谱特征对比

      数据引自:Yan et al.(2011)Duan et al.(2012)She et al.(2012)Wu et al.(2010)Xu et al.(2012)肖志斌(2012)李怀坤等(2013b)Wang et al.(2013)

      Fig.  9.  Detrital zircon U-Pb age relative probability diagrams plotted for comparison from Mid-Proterozoic strata of Dabie orogen, Shennongjia Group and Yangtze block

      图  10  大别地区中元古代“变砂岩-大理岩”组合与神农架群碎屑锆石Hf模式年龄TDM1TDM2对比

      神农架群数据肖志斌(2012)

      Fig.  10.  Distribution of detrital zircon Hf model ages of zircons from the Mesoproterozoic "metasandstone-marble" in Dabie area and Shennongjia Group

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    • 收稿日期:  2021-05-11
    • 网络出版日期:  2022-04-29
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