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    冀东青龙-双山子地区新太古代高镁安山岩-镁闪长岩锆石U-Pb年代学、地球化学及大地构造意义

    常青松 王惠初 荣桂林 初航 张健

    常青松, 王惠初, 荣桂林, 初航, 张健, 2019. 冀东青龙-双山子地区新太古代高镁安山岩-镁闪长岩锆石U-Pb年代学、地球化学及大地构造意义. 地球科学, 44(1): 23-36. doi: 10.3799/dqkx.2018.273
    引用本文: 常青松, 王惠初, 荣桂林, 初航, 张健, 2019. 冀东青龙-双山子地区新太古代高镁安山岩-镁闪长岩锆石U-Pb年代学、地球化学及大地构造意义. 地球科学, 44(1): 23-36. doi: 10.3799/dqkx.2018.273
    Chang Qingsong, Wang Huichu, Rong Guilin, Chu Hang, Zhang Jian, 2019. Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei. Earth Science, 44(1): 23-36. doi: 10.3799/dqkx.2018.273
    Citation: Chang Qingsong, Wang Huichu, Rong Guilin, Chu Hang, Zhang Jian, 2019. Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei. Earth Science, 44(1): 23-36. doi: 10.3799/dqkx.2018.273

    冀东青龙-双山子地区新太古代高镁安山岩-镁闪长岩锆石U-Pb年代学、地球化学及大地构造意义

    doi: 10.3799/dqkx.2018.273
    基金项目: 

    中国地质调查局地质调查项目 DD20160042

    国家自然科学基金面上项目 41572046

    详细信息
      作者简介:

      常青松(1985-), 男, 硕士, 工程师, 主要从事岩石学及地球化学方面的工作

      通讯作者:

      初航

    • 中图分类号: P581

    Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei

    • 摘要: 冀东地区位于华北克拉通北缘,学术界对该地区新太古代岩浆作用的成因模式及构造背景一直存在争议,因此对冀东青龙-双山子地区的新太古代变质表壳岩及侵入岩进行了系统的同位素年代学及岩石地球化学研究.锆石LA-MC-ICP-MS U-Pb年代学结果显示变安山岩的形成时代为2 576 Ma,辉长闪长岩-英云闪长岩-石英闪长岩的侵入时代为2 484~2 535 Ma.岩石地球化学特征显示,较早期的变安山岩部分属高镁安山岩类,源自俯冲板片脱水流体交代地幔楔的部分熔融;而稍晚的侵入岩类为具有埃达克质岩石特征的镁闪长岩类,源区具有熔体交代地幔楔部分熔融的特征;整体构成高镁安山岩-埃达克质镁闪长岩组合.结合区域上的同位素年代学及地球化学报道,冀东青龙-双山子地区新太古代应处于活动大陆边缘构造背景.

       

    • 图  1  大地构造简图及区域地质简图

      图 1a为大地构造单元划分简图,修改自Zhao et al.(2012)图 1b为遵化-青龙新太古代表壳岩及侵入岩分布,修改自Bai et al.(2016)Lu et al.(2017)Yang and Wei(2017);文献采样点郭荣荣等(2014)Bai et al.(2016)Guo et al.(2017)

      Fig.  1.  Tectonic and regional geological sketch

      图  2  研究区地质简图

      Fig.  2.  Geological sketch of study area

      图  3  正交偏光显微照片

      图 3a样品14JD20-1变安山岩;图 3b样品14JD20-4变玄武岩;图 3c样品14JD18-1变质辉长闪长岩;图 3d样品14JD17-1变质石英闪长岩.其中Pl.斜长石;Bi.黑云母;Px.辉石;Qtz.石英;Ser.绢云母

      Fig.  3.  Cross-polarized photomicrographs

      图  4  锆石阴极发光(CL)图像

      图 4a样品14JD16-1;图 4b样品14JD17-1;图 4c样品14JD23-1;图 4d样品14JD20-1.图中标示年龄为207Pb/206Pb年龄

      Fig.  4.  Zircon cathode luminescence (CL) images with 207Pb/206Pb ages

      图  5  锆石U-Pb谐和图

      图中灰色虚线椭圆为排除点

      Fig.  5.  Zircon U-Pb concordia diagrams

      图  6  岩石分类图解

      Fig.  6.  Rock classification diagrams

      图  7  岩浆岩TAS分类图解(a)及SiO2-FeOT/MgO图解(b)

      图a据Middlemost(1994);图b据邓晋福等(2010),TH.拉斑系列,CA.钙碱性系列,LF-CA.低Fe钙碱性系列

      Fig.  7.  TAS rock classification diagram (a) and SiO2-FeOT/MgO diagram (b)

      图  8  球粒陨石标准化稀土配分图解(a、c)及原始地幔标准化微量元素蜘蛛图解(b、d)

      图a、b为变火山岩样品;图c、d为变质侵入岩样品

      Fig.  8.  CHUR normalized REE distribution diagrams (a, c) and primitive mantle normalized spider diagrams (b, d)

      图  9  MgO-SiO2判别图解(a)和(La/Yb)N-K2O图解(b)

      图a底图据邓晋福等(2010),区域对比数据郭荣荣等(2014)Guo et al.(2015)Bai et al.(2016);图b底图据Martin et al.(2009),区域对比数据郭荣荣等(2014)Guo et al.(2015)Bai et al.(2016)

      Fig.  9.  MgO vs. SiO2 diagram (a) and (La/Yb)N vs. K2O diagram (b)

      图  10  (La/Yb)N-YbN图解(a)及S/Y-Y图解(b)

      图b据Martin(1999);区域对比数据郭荣荣等(2014)Guo et al.(2015)Bai et al.(2016)

      Fig.  10.  (La/Yb)N vs. YbN (a) and S/Y vs. Y (b) diagrams

      图  11  Nb/Y-La/Yb图解(a)及Sr/Y-Mg/(Mg+Fe)图解(b)

      图a据Martin et al.(2009);区域对比数据郭荣荣等(2014)Guo et al.(2015)Bai et al.(2016)

      Fig.  11.  Nb/Y vs. La/Yb (a) and Sr/Y vs. Mg/(Mg+Fe) (b) diagrams

      表  1  样品基本信息

      Table  1.   General information of samples

      采样单元 岩性 采样坐标 样品序号 测试手段
      双山子群鲁杖子组 变质安山岩 N40°19′49.05″;E119°08′39.92″ 14JD20-1 锆石U-Pb定年/地球化学
      变质安山岩 N40°19′49.05″;E119°08′39.92″ 14JD20-2 地球化学
      变质玄武岩 N40°19′49.05″;E119°08′39.92″ 14JD20-4 地球化学
      石英闪长玢岩 N40°20′04.61″;E119°08′35.99″ 14JD21-1 地球化学
      石英闪长玢岩 N40°20′04.61″;E119°08′35.99″ 14JD21-3 地球化学
      朱杖子群褚杖子组 斜长角闪变粒岩 N40°29′26.28″;E119°14′17.56″ 14JD28 地球化学
      变质侵入岩 变质中细粒英云闪长岩 N40°20′20.54″;E119°10′07.07″ 14JD16-1 锆石U-Pb定年/地球化学
      变质中细粒石英闪长岩 N40°21′39.16″;E119°09′28.48″ 14JD17-1 锆石U-Pb定年/地球化学
      变质细粒辉长闪长岩 N40°20′31.80″;E119°08′45.20″ 14JD18-1 地球化学
      变质细粒辉长闪长岩 N40°20′31.80″;E119°08′45.20″ 14JD18-2 地球化学
      变质细粒石英闪长岩 N40°19′38.18″;E119°07′29.44″ 14JD23-1 锆石U-Pb定年/地球化学
      变质细粒石英闪长岩 N40°19′38.18″;E119°07′29.44″ 14JD23-2 地球化学
      变质石英闪长玢岩 N40°17′35.73″;E119°06′12.49″ 14JD25-1 地球化学
      下载: 导出CSV
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