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    内蒙古宝音图-霍各乞地区宝音图岩群的时代约束及构造属性

    滕飞 滕学建 刘洋 何鹏 郭硕 王文龙 田健 段霄龙

    滕飞, 滕学建, 刘洋, 何鹏, 郭硕, 王文龙, 田健, 段霄龙, 2019. 内蒙古宝音图-霍各乞地区宝音图岩群的时代约束及构造属性. 地球科学, 44(1): 161-178. doi: 10.3799/dqkx.2018.240
    引用本文: 滕飞, 滕学建, 刘洋, 何鹏, 郭硕, 王文龙, 田健, 段霄龙, 2019. 内蒙古宝音图-霍各乞地区宝音图岩群的时代约束及构造属性. 地球科学, 44(1): 161-178. doi: 10.3799/dqkx.2018.240
    Teng Fei, Teng Xuejian, Liu Yang, He Peng, Guo Shuo, Wang Wenlong, Tian Jian, Duan Xiaolong, 2019. Geochronological Constraint on the Baoyintu Group and Its Tectonic Significance in Baoyintu-Huogeqi Area, Inner Mongolia. Earth Science, 44(1): 161-178. doi: 10.3799/dqkx.2018.240
    Citation: Teng Fei, Teng Xuejian, Liu Yang, He Peng, Guo Shuo, Wang Wenlong, Tian Jian, Duan Xiaolong, 2019. Geochronological Constraint on the Baoyintu Group and Its Tectonic Significance in Baoyintu-Huogeqi Area, Inner Mongolia. Earth Science, 44(1): 161-178. doi: 10.3799/dqkx.2018.240

    内蒙古宝音图-霍各乞地区宝音图岩群的时代约束及构造属性

    doi: 10.3799/dqkx.2018.240
    基金项目: 

    中国地质调查局地质调查项目 12120113056300

    详细信息
      作者简介:

      滕飞(1987-), 男, 工程师, 主要工作为构造地质及区域地质

    • 中图分类号: P581

    Geochronological Constraint on the Baoyintu Group and Its Tectonic Significance in Baoyintu-Huogeqi Area, Inner Mongolia

    • 摘要: 宝音图隆起的构造归属仍然存在争议,有学者认为是兴蒙造山带中的微陆块,也有观点认为是华北克拉通的一部分.作为宝音图隆起的重要组成部分,探究宝音图岩群的形成时代、构造归属是解决这一问题的重要途径.通过对宝音图岩群3件石英岩样品进行锆石U-Pb同位素测试,在一岩组(石英岩和石英片岩岩组)、二岩组(石英岩岩组)、三岩组(片岩岩组)中分别获得较可靠的碎屑锆石最小谐和年龄为1 284 Ma、1 319 Ma、1 395 Ma,代表各岩组的沉积上限.结合侵入宝音图岩群中的变质基性脉岩的锆石U-Pb年龄为895.5±6.8 Ma,将研究区宝音图岩群一-三岩组的沉积时代大致限定在895.5~1 284.0 Ma之间,位于中元古代晚期至新元古代早期;可以和相邻区域大致形成于同一时期的阿拉善地区阿拉善群、白云鄂博地区白云鄂博群上亚群、化德-康保地区化德群上亚群对比.斜长角闪岩地球化学特征反映其形成于大陆边缘裂谷环境,可能为Rodinia超大陆裂解在本区的响应.宝音图岩群与邻区同时代沉积建造的碎屑锆石年龄谱较为相似,其主要峰值反映的地质事件与华北克拉通所经历的主要构造-热事件可以较好对应,说明宝音图岩群的物源来自于华北克拉通,为华北克拉通边缘的沉积.宝音图隆起应当为华北的一部分.

       

    • 图  1  内蒙古狼山北部地质图及采样位置

      a.中亚造山带构造简图,据Jahn et al.(2000);b.宝音图隆起构造位置,据Hu et al.(2014);c.研究区地质简图,据河北省区域地质矿产调查研究所, 2012, 内蒙古1:25万巴音查干幅区域地质调查报告,以及Hu et al.(2014)Wang et al.(2016)王文龙等(2017)

      Fig.  1.  The geological sketch and sample localities of northern Langshan area, Inner Mongolia

      图  2  宝音图岩群地层柱状图

      底图据内蒙古地质矿产局(1991)以及中国地质调查局天津地质调查中心, 2016, 内蒙古1:5万查干呼舒庙幅、楚鲁庙幅、潮格幅、哈尔木格台幅、那仁宝力格公社幅、居力格台幅区域地质矿产调查报告; 样品10TW58数据孙立新等(2013)

      Fig.  2.  Stratigraphic column of the Baoyintu Grou

      图  3  宝音图岩群实测剖面

      剖面位置见图 1c;图例同图 2

      Fig.  3.  Sections of the Baoyintu Group

      图  4  宝音图岩群样品露头及镜下特征

      a~b.浅灰色石榴(十字)云母片岩夹石英岩露头及样品14QDM-1灰白色石英岩正交偏光镜下特征;c~d.石英岩夹少量云母石英片岩露头及样品6017-4灰白色石英岩正交偏光镜下特征;e~f.云母石英片岩与石英岩互层露头及样品P2TW55-1浅灰色含二云石英岩正交偏光镜下特征;g~h.样品6021-1灰黑色含石榴斜长角闪(片)岩露头及正交偏光镜下特征

      Fig.  4.  Outcrop photos and photomicrographs of the Baoyintu Group

      图  5  宝音图岩群斜长角闪岩判别图解

      a.(al+fm)-(c+alk)-Si图解,据Simone(1953);b.MgO-CaO-FeO*图解,据Walker et al.(1960);c.TiO2-Zr/P2O5图解,据Winchester and Floyd(1976);d.Zr/TiO2-Nb/Y图解,据Winchester and Floyd(1977);e.稀土元素蛛网图,据Sun and McDonough(1989);f.微量元素蛛网图,据Sun and McDonough(1989);g.Th/Zr-Nb/Zr图解,据孙书勤和汪云亮(2003);h.Th/Hf-Ta/Hf图解,据汪云亮等(2001);i.Y/15-La/10-Nb/8图解,据Campbell et al.(1990);1A区为钙碱性玄武岩;1C区为火山弧拉斑玄武岩;1B区为1A区和1C区的重叠区域;2A区为大陆玄武岩;2B区为弧后盆地大陆玄武岩;3A区为大陆内裂谷区的碱性玄武岩;3B和3C区为富集型洋脊玄武岩;3D区为正常洋脊玄武岩

      Fig.  5.  Discrimination diagrams of the amphibolite in the Baoyintu Group

      图  6  部分锆石CL图像

      Fig.  6.  Representative selection of cathodoluminescence (CL) zircon images

      图  7  宝音图岩群石英岩碎屑锆石年龄直方图

      Fig.  7.  Comparison of detrital zircon age patterns of quarzite from Baoyintu Group

      图  8  宝音图岩群石榴斜长角闪岩锆石U-Pb年龄谐和图

      Fig.  8.  Zircon U-Pb concordia diagrams for the amphibolite sample from the Baoyintu Group

      图  9  华北克拉通北缘中—新元古代地层对比

      蓝色代表碎屑锆石年龄(Ma),红色代表花岗岩或岩墙年龄(Ma),绿色代表斑脱岩、火山岩地层年龄(Ma).阿拉善地区的年龄数据肖志斌等(2015);狼山地区狼山群数据引自Hu et al.(2014);渣尔泰山地区年龄数据公王斌等(2016);白云鄂博地区的数据钟焱(2015);化德地区的数据胡波等(2009)Liu et al.(2014);燕辽地区的数据转李怀坤等(2014)任荣等(2011)

      Fig.  9.  Stratigraphic correlation of northern margin of the North China Craton

      图  10  宝音图岩群及邻区同时代地层U-Pb年龄直方图

      Fig.  10.  The comparison of the probability density distribution plots of the U-Pb age

      表  1  宝音图岩群斜长角闪岩地球化学数据

      Table  1.   Analysis results of major elements, trace elements and rare earth elements of the amphibolite in the Baoyintu Group

      样号 SiO2 Al2O3 Fe2O3 FeO CaO MgO K2O Na2O TiO2 P2O5 MnO los
      6021-1 49.63 16.77 1.99 10.21 7.88 5.70 0.37 2.99 2.00 0.17 0.23 0.72
      样号 H2O+ Cu Pb Zn Cr Ni Co Li Rb Cs Sr Ba
      6021-1 0.50 39.7 45.3 196 80.0 19.4 35.6 34.2 15.4 0.44 210 95.2
      样号 SiO2 Al2O3 Fe2O3 FeO CaO MgO K2O Na2O TiO2 P2O5 MnO los
      6021-2 50.30 15.98 3.33 9.06 8.02 5.73 0.32 3.06 1.88 0.17 0.21 0.73
      样号 H2O+ Cu Pb Zn Cr Ni Co Li Rb Cs Sr Ba
      6021-2 0.61 46.2 49.4 162 79.2 24.4 36.7 33.9 10.8 0.35 224 59.5
      样号 V Sc Nb Ta Zr Hf Ga U Th La Ce Pr
      6021-1 268 37.7 7.56 0.64 153 4.75 23.5 2.11 2.91 10.4 22.1 3.40
      样号 Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Y
      6021-1 15.4 4.44 1.72 4.83 1.01 6.40 1.33 3.85 0.58 3.66 0.55 34.0
      样号 V Sc Nb Ta Zr Hf Ga U Th La Ce Pr
      6021-2 266 31.0 7.60 0.61 110 3.60 21.9 1.69 2.46 10.8 23.2 3.65
      样号 Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Y
      6021-2 16.9 4.59 1.53 4.80 0.99 6.18 1.25 3.54 0.51 3.32 0.51 31.6
      注:主量元素单位为%,微量、稀土元素单位为10-6.
      下载: 导出CSV
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