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    内蒙古科右中旗两类基性岩的年代学、地球化学及其构造意义

    金松 李英杰 钱程 张杨 孟都 杨海波 王博 伍光锋

    金松, 李英杰, 钱程, 张杨, 孟都, 杨海波, 王博, 伍光锋, 2022. 内蒙古科右中旗两类基性岩的年代学、地球化学及其构造意义. 地球科学, 47(1): 342-356. doi: 10.3799/dqkx.2021.051
    引用本文: 金松, 李英杰, 钱程, 张杨, 孟都, 杨海波, 王博, 伍光锋, 2022. 内蒙古科右中旗两类基性岩的年代学、地球化学及其构造意义. 地球科学, 47(1): 342-356. doi: 10.3799/dqkx.2021.051
    Jin Song, Li Yingjie, Qian Cheng, Zhang Yang, Meng Du, Yang Haibo, Wang Bo, Wu Guangfeng, 2022. Geochronology and Geochemistry of Two Types of Basic Rocks in Horqin Right Middle Banner, Inner Mongolia and Their Tectonic Significances. Earth Science, 47(1): 342-356. doi: 10.3799/dqkx.2021.051
    Citation: Jin Song, Li Yingjie, Qian Cheng, Zhang Yang, Meng Du, Yang Haibo, Wang Bo, Wu Guangfeng, 2022. Geochronology and Geochemistry of Two Types of Basic Rocks in Horqin Right Middle Banner, Inner Mongolia and Their Tectonic Significances. Earth Science, 47(1): 342-356. doi: 10.3799/dqkx.2021.051

    内蒙古科右中旗两类基性岩的年代学、地球化学及其构造意义

    doi: 10.3799/dqkx.2021.051
    基金项目: 

    国家自然科学基金项目 41972061

    中国地质调查局项目 DD20160048-14

    详细信息
      作者简介:

      金松(1988-), 男, 硕士研究生, 矿物学、岩石学、矿床学专业.ORCID: 0000-0003-4441-1322.E-mail: 732818885@qq.com

      通讯作者:

      李英杰, E-mail: liyingjie820@126.com

    • 中图分类号: P534.51;P534.46

    Geochronology and Geochemistry of Two Types of Basic Rocks in Horqin Right Middle Banner, Inner Mongolia and Their Tectonic Significances

    • 摘要:

      兴蒙造山带东段晚古生代构造演化存在争议,基性岩浆作用是构造演化过程中的良好地质记录. 对贺根山缝合带东段内蒙古科右中旗构造混杂岩带内的杜尔基基性岩和甲哈达基性岩进行了系统的地质特征、岩相学、年代学和地球化学研究. 杜尔基基性岩岩性为枕状玄武岩和辉绿岩,辉绿岩锆石LA-ICP-MS U-Pb年龄为348.3±2.6 Ma,为低钾拉斑玄武系列,相对富集LILE,亏损Nb、Ta等高场强元素. 甲哈达基性岩岩性主要为玄武岩,锆石U-Pb年龄为317.6±3.0 Ma,为钙碱性系列,同样具有HFSE亏损和LILE富集的特点,与杜尔基基性岩相比更加富集LILE和LREE. 结合贺根山缝合带早石炭世蛇绿岩及洋内俯冲作用的研究成果,认为从杜尔基基性岩到甲哈达基性岩的演化,可能指示了古亚洲洋东段早-晚石炭世洋内俯冲的渐进过程,洋内弧从不成熟向逐渐成熟演化.

       

    • 图  1  研究区大地构造位置和地质简图

      a. 据Xiao et al. (2009)修改;b. 据肖文交等(2019)修改. 1.上二叠统;2.下二叠统;3.上侏罗统;4.下白垩统;5.第四系;6.早白垩世花岗岩;7.晚侏罗世花岗岩;8.晚三叠世花岗岩;9.甲哈达基性岩;10.杜尔基基性岩;11.断层界线/角度不整合界线;12.样品采集位置

      Fig.  1.  Geological map showing the tectonic units and geological sketch map of the study area

      图  2  杜尔基基性岩野外露头及镜下特征

      a. 玄武岩与变质粉砂岩基质断层接触;b. 玄武岩枕状构造;c. 斑状玄武岩镜下特征;d. 无斑玄武岩镜下特征;e. 辉绿岩野外特征;f. 辉绿岩镜下特征. Ab.钠长石;Act.阳起石;Pl.斜长石;Cpx.单斜辉石

      Fig.  2.  The field and microscopic features of basic rocks in Duerji

      图  3  甲哈达基性岩野外露头及镜下特征

      a. 玄武岩构造变形特征;b. 玄武岩上覆薄层状泥质硅质岩;c. 透辉橄榄玄武岩镜下特征;d. 球颗玄武岩镜下特征. Ol.橄榄石;Di.透辉石;Pl.斜长石;Cb.碳酸盐

      Fig.  3.  The field and microscopic features of basic rocks in Jiahada

      图  4  科右中旗两类基性岩典型锆石CL图像和LA-ICP-MS U-Pb谐和图

      a、b. 杜尔基辉绿岩;c、d.甲哈达玄武岩

      Fig.  4.  CL images and LA-ICP-MS U-Pb concordia diagrams of typical zircons from two types of basic rocks in Horqin Right Middle Banner

      图  5  科右中旗两类基性岩岩石分类命名及岩浆系列判别图解

      Fig.  5.  Classification of rocks and magma series discrimination of two types of basic rocks in Horqin Right Middle Banner

      图  6  科右中旗两类基性岩和全球典型玄武岩的稀土元素球粒陨石标准化配分模式和微量元素原始地幔标准化蛛网图

      Sun and McDonough(1989)Schmidt and Jagoutz(2017)

      Fig.  6.  Chondrite-normalized REE distribution patterns and primitive mantle-normalized trace element spidergrams of two types of basic rocks in Horqin Right Middle Banner and global typical basalts

      图  7  科右中旗两类基性岩构造环境判别图解

      图a据Wood(1980);图b据Pearce(20082014). IAT.岛弧拉斑系列;CAB.岛弧钙碱性系列;N-MORB.正常洋中脊玄武岩;E-MORB.富集洋中脊玄武岩;WPT.板内玄武岩;OIB.洋岛玄武岩;WPAB.板内碱性玄武岩

      Fig.  7.  Tectonic discrimination diagrams of two types of basic rocks in Horqin Right Middle Banner

      图  8  科右中旗洋内弧岩石组合剖面、西乌旗迪彦庙前弧玄武岩剖面和伊豆‒小笠原‒马里亚纳(IBM)前弧岩石地层剖面对比

      a. 据Ishizuka et al. (2014);b. 据李英杰等(2018)

      Fig.  8.  The comparison between the FAB in the Diyanmiao ophiolite, Izu-Bonin-Mariana forearc rock stratigraphic section and intra⁃oceanic arc sequence in Horqin Right Middle Banner

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    出版历程
    • 收稿日期:  2021-02-08
    • 网络出版日期:  2022-02-11
    • 刊出日期:  2022-01-20

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