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    内蒙古迪彦庙孬来可图侵入岩的年代学、Sr-Nd-Hf同位素特征及其地质意义

    范玉须 肖庆辉 程杨 李岩 刘勇 郭灵俊 庞进力

    范玉须, 肖庆辉, 程杨, 李岩, 刘勇, 郭灵俊, 庞进力, 2020. 内蒙古迪彦庙孬来可图侵入岩的年代学、Sr-Nd-Hf同位素特征及其地质意义. 地球科学, 45(7): 2379-2392. doi: 10.3799/dqkx.2020.100
    引用本文: 范玉须, 肖庆辉, 程杨, 李岩, 刘勇, 郭灵俊, 庞进力, 2020. 内蒙古迪彦庙孬来可图侵入岩的年代学、Sr-Nd-Hf同位素特征及其地质意义. 地球科学, 45(7): 2379-2392. doi: 10.3799/dqkx.2020.100
    Fan Yuxu, Xiao Qinghui, Cheng Yang, Li Yan, Liu Yong, Guo Lingjun, Pang Jinli, 2020. Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia. Earth Science, 45(7): 2379-2392. doi: 10.3799/dqkx.2020.100
    Citation: Fan Yuxu, Xiao Qinghui, Cheng Yang, Li Yan, Liu Yong, Guo Lingjun, Pang Jinli, 2020. Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia. Earth Science, 45(7): 2379-2392. doi: 10.3799/dqkx.2020.100

    内蒙古迪彦庙孬来可图侵入岩的年代学、Sr-Nd-Hf同位素特征及其地质意义

    doi: 10.3799/dqkx.2020.100
    基金项目: 

    内蒙古自治区地质矿产勘查基金项目 2017-YS01

    中国地质调查项目 DD20160345

    详细信息
      作者简介:

      范玉须(1987-), 男, 博士, 主要从事构造地质学与成矿研究.ORCID:0000-0001-7721-7003.E-mail:562442919@qq.com

      通讯作者:

      肖庆辉, ORCID:0000-0002-8539-7574.E-mail:qinghuixiao@126.com

    • 中图分类号: P58

    Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia

    • 摘要: 以内蒙古迪彦庙蛇绿混杂岩带中的孬来可图侵入岩体为研究对象,通过详细的岩石学、年代学以及Sr-Nd-Hf同位素特征分析,探讨岩石成因及构造环境.岩体的锆石U-Pb年龄为322.2±1.3 Ma,表明该岩体属晚石炭世早期岩浆活动的产物.岩石化学成分中SiO2含量较高(62.29%~77.17%);Al2O3含量较低(11.45%~14.11%),属准铝质岩浆系列;富钠贫钾(Na2O=2.91%~3.84%,K2O=0.54%~1.79%),同时富集大离子亲石元素而亏损高场强元素,具有TTG的地球化学特征.岩石稀土元素含量较低,轻、重稀土分异不明显,具中等强度的负Eu异常(δEu=0.64~0.76).岩石的εHft)值均为正,介于+8.1~+13.3之间,模式年龄相对年轻,同时(87Sr/86Sr)i较低(0.703 457~0.703 789),εNdt)均为正值(+8.4~+9.3),具有MORB源区的特征,推测岩浆起源于古亚洲洋俯冲洋壳.结合西乌旗岩浆弧中不同源区的TTG岩类分析,石炭纪,古亚洲洋在西乌旗地区尚未关闭,而是处于热壳-热幔的壳幔构造背景中,洋壳俯冲消减,岩浆侵位,陆壳增生.

       

    • 图  1  (a) 区域构造简图(据Xiao et al., 2003修改);(b)孬来可图区域地质简图

      Fig.  1.  (a) Sketch tectonic map(modified from Xiao et al., 2003); (b) Regional geological map of Naolaiketu

      图  2  孬来可图侵入岩野外及镜下照片

      a, b.侵入岩的野外宏观照片;c, d.岩石的镜下显微特征(比例尺为500 μm)

      Fig.  2.  Field photographs and photomicrographs of the plutonic rocks, in Naolaiketu

      图  7  岩石的An-Ab-Or分类图解和K-Na-Ca图解

      Tn.英云闪长岩;Tr.奥长花岗岩;Gd.花岗闪长岩;MG.二长花岗岩;Gr.花岗岩;a.据O'Connor(1965);b.据Martin et al.(2005)

      Fig.  7.  An-Ab-Or diagram (a) and K-Na-Ca diagram(b)

      图  3  孬来可图石英闪长岩锆石阴极发光图、分析点和年龄

      Fig.  3.  Representative CL images of analyzed zircons, ages and analysis spots (cycle) are marked on the zircons

      图  4  孬来可图岩体锆石U-Pb年龄协和图

      Fig.  4.  Zircon U-Pb concordia diagrams for Naolaiketu pluton

      图  5  孬来可图岩石的K2O-SiO2图(a.据Peccerillo and Taylor, 1976),ANK-ACNK图解(b.据Maniar and Piccoli, 1989)

      Fig.  5.  (a) K2O-SiO2 (modified from Peccerillo and Taylor, 1976) and (b) ANK-ACNK plot(modified from Maniar and Piccoli, 1989)

      图  6  岩石的REE元素球粒陨石标准化图解及微量元素原始地幔标准化蛛网图

      标准化数据据文献Sun and McDonough(1989)

      Fig.  6.  Chondrite-normalized REE pattern and primitive mantle-normalized trace elements spider diagram

      图  8  (a) 孬来可图岩石Rb-(Y+Nb)构造判别图解和(b)Rb-(Yb+Ta)图解(据Pearce et al., 1984)

      Fig.  8.  (a)Rb-(Y+Nb) and (b)Rb-(Yb+Ta) tectonic discriminate diagrams of the Naolaiketu(modified from Pearce et al., 1984)

      图  9  TTG岩C/MF-A/MF图

      Altherr et al.(2002)

      Fig.  9.  C/MF-A/MF diagram of TTG

      图  10  (87Sr/86Sr)iNd(t)同位素组成图解

      底图据Hou et al.(2004);迪彦庙蛇绿岩数据来自程杨等(2019)

      Fig.  10.  (87Sr/86Sr)iNd(t) isotope composition of Naolaiketu

      图  11  锆石εHf(t)-T图解(据Yang et al., 2006)

      Fig.  11.  εHf(t)-T diagram of zircon(modified from Yang et al., 2006)

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