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    兴蒙造山带南缘早古生代增生造山带内前寒武纪地层的识别及其地质意义

    杨泽黎 胡晓佳 王树庆 王文龙 赵利刚 段霄龙 田健 程银行

    杨泽黎, 胡晓佳, 王树庆, 王文龙, 赵利刚, 段霄龙, 田健, 程银行, 2021. 兴蒙造山带南缘早古生代增生造山带内前寒武纪地层的识别及其地质意义. 地球科学, 46(8): 2786-2803. doi: 10.3799/dqkx.2020.281
    引用本文: 杨泽黎, 胡晓佳, 王树庆, 王文龙, 赵利刚, 段霄龙, 田健, 程银行, 2021. 兴蒙造山带南缘早古生代增生造山带内前寒武纪地层的识别及其地质意义. 地球科学, 46(8): 2786-2803. doi: 10.3799/dqkx.2020.281
    Yang Zeli, Hu Xiaojia, Wang Shuqin, Wang Wenlong, Zhao Ligang, Duan Xiaolong, Tian Jian, Cheng Yinhang, 2021. Identification of Precambrian Strata in Early Paleozoic Accretion Zone on Southern Margin of Xing-Meng Orogenic Belt and Its geological Significance. Earth Science, 46(8): 2786-2803. doi: 10.3799/dqkx.2020.281
    Citation: Yang Zeli, Hu Xiaojia, Wang Shuqin, Wang Wenlong, Zhao Ligang, Duan Xiaolong, Tian Jian, Cheng Yinhang, 2021. Identification of Precambrian Strata in Early Paleozoic Accretion Zone on Southern Margin of Xing-Meng Orogenic Belt and Its geological Significance. Earth Science, 46(8): 2786-2803. doi: 10.3799/dqkx.2020.281

    兴蒙造山带南缘早古生代增生造山带内前寒武纪地层的识别及其地质意义

    doi: 10.3799/dqkx.2020.281
    基金项目: 

    中国地质调查局项目 DD20190038

    国家自然科学基金项目 41872068

    详细信息
      作者简介:

      杨泽黎(1989-), 男, 硕士, 工程师, 主要从事岩石学研究及地质调查工作.ORCID: 0000-0001-5559-6102.E-mail: 812295251@qq.com

      通讯作者:

      胡晓佳, E-mail: 278558023@qq.com

    • 中图分类号: P588.21

    Identification of Precambrian Strata in Early Paleozoic Accretion Zone on Southern Margin of Xing-Meng Orogenic Belt and Its geological Significance

    • 摘要: 兴蒙造山带南缘早古生代增生造山带内是否存在陆壳一直缺少直接证据,制约了对增生带结构及演化的认识.在达茂旗东北部兴蒙造山带南缘增生带内识别出一套原地的变质地层,野外观察及锆石U-Pb年代学、Hf同位素地球化学研究表明,该套地层形成时代为中元古代晚期,可能代表了增生造山带内的古老地壳.地层的碎屑锆石峰值年龄集中于~1.8 Ga,并具有~3.0 Ga、~2.8 Ga、~2.5 Ga、~1.6 Ga等次级峰值,与华北北缘白云鄂博、化德、狼山群等地层碎屑锆石年龄组成一致;表明其应为华北陆块的一部分,物源则主要来自于华北克拉通内部不同时代地质体的剥蚀.该套地层的识别及其与华北陆块的亲缘性表明,早古生代兴蒙造山带南缘增生带内存在陆壳,构造环境上应为古亚洲洋向华北克拉通俯冲形成的活动陆缘;同时,其与车根达来构造带的关系显示后者并非蛇绿岩,更可能为弧后伸展引起的超基性岩对陆壳的侵入形成.

       

    • 图  1  研究区构造位置(a)、构造单元划分(b)及地质简图(c)

      图a据Liu et al.(2017b)He et al.(2018);图b据Xiao et al.(2003)Li et al.(2014);图c修改自张维和简平(2008)

      Fig.  1.  Tectonic location (a), division of tectonic units (b) and geological sketch map (c) of the study area

      图  2  达茂旗车根达来地区前寒武纪地层野外地质剖面

      Fig.  2.  Geological section of Precambrian strata in Chegendalai area, Damaoqi

      图  3  达茂旗车根达来地区前寒武纪地层野外特征

      a~c. 地层被早古生代岩体侵入;d、e. 前寒武纪地层不同成分层特征;f. 地层糜棱岩化变形

      Fig.  3.  Field photos of Precambrian strata in Chegendalai area, Damaoqi

      图  4  样品野外特征及岩相学显微照片

      a、b. 石英岩;c、d. 含石榴石黑云角闪片岩;e、f. 含石榴石绢云石英片岩.Qz.石英;Grt.石榴石;Amp.角闪石;Bi.黑云母;Ms.白云母

      Fig.  4.  Field outcrop and microphotographs of the Precambrian strata

      图  5  车根达来前寒武纪地层锆石CL图像、LA-ICP-MS分析点位、207Pb/206Pb年龄及εHf(t)值

      Fig.  5.  CL images, localities of the points for LA-ICP-MS measurement, 207Pb/206Pb ages and εHf(t) values of zircons from the Precambrian strata in Chegendalai area

      图  6  车根达来前寒武纪地层锆石U-Pb谐和图(a、c、e)及年龄分布图(b、d、f)

      Fig.  6.  U-Pb concordia diagrams (a, c, e) and probability density plots (b, d, f) of zircons from the Precambrian strata in Chegendalai area

      图  7  车根达来前寒武纪地层锆石t-εHf(t)关系(a)及模式年龄分布直方图(b~d)

      Fig.  7.  t-εHf(t) diagram (a) and two-stage Hf model age (TDM2) histograms (b-d) of the Precambrian strata in Chegendalai area, Damaoqi

      图  8  车根达来前寒武纪地层、白云鄂博群、化德群、狼山群沉积岩碎屑锆石年龄组成对比

      a. 车根达来前寒武纪地层碎屑锆石年龄组成;b. 白云鄂博群碎屑锆石年龄组成(数据引自Liu et al., 2017aZhou et al., 2017);c. 化德群碎屑锆石年龄组成(数据引自Liu et al., 2014, 2018);d. 狼山群碎屑锆石年龄组成(数据引自Hu et al., 2014

      Fig.  8.  Comparison of detrital zircon U-Pb ages from different strata

      图  9  兴蒙造山带南缘早古生代构造演化模式

      Fig.  9.  Early Paleozoic tectonic evolution model of the southern margin of Xing-Meng Orogenic Belt

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