冀北单塔子群凤凰嘴杂岩的年代学研究

曲军峰, 李锦轶, 刘建峰. 2012. 冀北单塔子群凤凰嘴杂岩的年代学研究. 岩石学报, 28(9): 2879-2889.
引用本文: 曲军峰, 李锦轶, 刘建峰. 2012. 冀北单塔子群凤凰嘴杂岩的年代学研究. 岩石学报, 28(9): 2879-2889.
QU JunFeng, LI JinYi, LIU JianFeng. 2012. Geochronological study on the Fenghuangzui complex of Dantazi Group at northern Hebei Province. Acta Petrologica Sinica, 28(9): 2879-2889.
Citation: QU JunFeng, LI JinYi, LIU JianFeng. 2012. Geochronological study on the Fenghuangzui complex of Dantazi Group at northern Hebei Province. Acta Petrologica Sinica, 28(9): 2879-2889.

冀北单塔子群凤凰嘴杂岩的年代学研究

  • 基金项目:

    本文受中国地质调查局地质调查工作项目(1212011085476); 国家自然科学基金(40872058)和地科院地质所所长基金联合资助

详细信息
    作者简介:

    曲军峰, 男, 1979年生, 博士, 副研究员, 岩石学专业, E-mail: qujf@cags.ac.cn

  • 中图分类号: P588.121;P588.124;P597.3

Geochronological study on the Fenghuangzui complex of Dantazi Group at northern Hebei Province

  • 冀北地区基底的研究对理解华北克拉通早前寒武纪的演化具有重要意义。本文通过对冀北地区单塔子群凤凰嘴杂岩的锆石年代学工作探讨早前寒武纪华北克拉通北缘所经历的构造事件。单塔子群凤凰嘴杂岩主要由糜棱岩化的花岗质片麻岩和侵入其中的变质的基性岩墙组成。其中花岗质片麻岩的锆石呈明显的核边结构, 岩浆核的谐和年龄为2.45Ga, 变质边的年龄为1.95Ga。变质岩墙中的锆石未见明显的核边结构, 阴极发光照片显示为变质锆石的特征, 得到的年龄为1.9Ga。此年龄与花岗质片麻岩锆石的变质年龄相似, 说明二者共同经历了古元古代的造山事件。此外, 尽管没有得到岩墙的确切形成时代, 但单塔子群内普遍发育的大规模岩墙说明在2.54~1.9Ga之间, 该区经历了一次规模较大的伸展事件。

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  • 图 1 

    冀北地区前寒武纪变质杂岩地质简图(据刘树文等, 2007a修改)

    Figure 1. 

    Geological map of the Precambrian metamorphic complexes in northern Hebei (after Liu et al., 2007a)

    图 2 

    承德地区单塔子群地质简图

    Figure 2. 

    Geological map of distribution of the Dantazi Group in Chengde

    图 3 

    凤凰嘴杂岩野外露头

    Figure 3. 

    Field photographs of the Fenghuangzui Complex

    图 4 

    凤凰嘴杂岩显微结构照片

    Figure 4. 

    Microphotographs of the Fenghuangzui complex

    图 5 

    变基性岩样品TD89-5 CL图像及部分定年结果

    Figure 5. 

    Representative cathodoluminescence (CL) images of zircon from the sample TD89-5

    图 6 

    样品TD89-5锆石U-Pb同位素谐和线图

    Figure 6. 

    U-Pb isotopic concordia diagram of sample TD89-5

    图 7 

    样品TD89-4 CL图像及部分定年结果

    Figure 7. 

    Representative cathodoluminescence (CL) images of zircon from the sample TD89-4

    图 8 

    样品TD89-4锆石U-Pb同位素谐和线图

    Figure 8. 

    U-Pb isotopic concordia diagram of sample TD89-4

    图 9 

    激光剥蚀后花岗片麻岩样品TD89-4锆石CL图像

    Figure 9. 

    Representative cathodoluminescence (CL) images of zircon from the sample TD89-4

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出版历程
收稿日期:  2011-10-08
修回日期:  2012-02-27
刊出日期:  2012-09-01

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