首页> 外文期刊>International Journal of Earth Sciences >Timing of left-lateral shearing along the Ailao Shan-Red River shear zone: constraints from zircon U-Pb ages from granitic rocks in the shear zone along the Ailao Shan Range, Western Yunnan,China
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Timing of left-lateral shearing along the Ailao Shan-Red River shear zone: constraints from zircon U-Pb ages from granitic rocks in the shear zone along the Ailao Shan Range, Western Yunnan,China

机译:沿哀牢山-红河剪切带左旋剪切的时机:云南西部哀牢山剪切带的花岗岩中锆石U-Pb年龄限制

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摘要

As the boundary between the Indochina and the South China blocks, the Ailao Shan-Red River (ASRR) shear zone underwent a sinistral strike-slip shearing which is characterized by ductile deformation structures along the Ailao Shan range. The timing issue of left-lateral shearing along the ASRR shear zone is of first-order importance in constraining the nature and regional significance of the shear zone. It has been, therefore, focused on by many previous studies, but debates still exist on the age of initiation and termination of shearing along the shear zone. In this paper, we dated 5 samples of granitic plutons (dykes) along the Ailao Shan shear zone. Zircon U-Pb ages of four sheared or partly sheared granitic rocks give ages of 30.9 ± 0.7, 36.6 ±0.1, 25.9 ± 1.0 and 27.2 ± 0.2 Ma, respectively. An undeformed granitic dyke intruding mylonitic foliation gives crystallization age of 21.8 ± 1 Ma. The Th/U ratios of zircon grains from these rocks fall into two populations (0.17-1.01 and 0.07-0.08), reflecting magmatic and metamorphic origins of the zircons. Detailed structural and microstructural analysis reveals that the granitic intrusions are ascribed to pre-, syn- and post-shearing magmatisms. The zircon U-Pb ages of these granites provide constraints on timing of the initiation (later than 31 Ma from pre-shearing granitic plutons, but earlier than 27 Ma from syn-shearing granitic dykes) and termination (ca. 21 Ma from the post-shearing granitic dykes) of strong ductile left-lateral shearing, which is consistent with previous results on the Diancang Shan and Day Nui Con Voi massifs in the literature. We also conclude that the left-lateral shearing along the ASRR shear zone is the result of southeastward extrusion of the Indochina block during the Indian-Eurasian plate collision. Furthermore, the left-lateral shearing was accompanied by the ridge jump, postdating the opening, of the South China Sea.
机译:作为印度支那和华南地块之间的边界,哀牢山-红河(ASRR)剪切带经历了一条左旋走滑剪切,其特征是沿着哀牢山山脉的韧性变形结构。沿ASRR剪切带左旋剪切的时间问题对于限制剪切带的性质和区域意义具有重要意义。因此,以前的许多研究都把重点放在了这个问题上,但是关于沿剪切带剪切的起始和终止的年龄仍然存在争议。在本文中,我们对哀牢山剪切带上的5个花岗岩类岩体(堤)进行了测年。四个剪切或部分剪切的花岗岩岩石的锆石U-Pb年龄分别为30.9±0.7、36.6±0.1、25.9±1.0和27.2±0.2 Ma。一个未变形的花岗岩堤侵入到淀粉状的叶脉中,结晶年龄为21.8±1 Ma。这些岩石中锆石的Th / U比值分为两个总体(0.17-1.01和0.07-0.08),反映了锆石的岩浆和变质成因。详细的结构和微观结构分析表明,花岗岩的侵入是由于剪切前,同理和剪切后的岩浆作用引起的。这些花岗岩的锆石U-Pb年龄限制了起始时间(预剪切花岗质岩岩层大于31 Ma,但同向剪切花岗岩岩层年龄大于27 Ma)和终止时间(后期约21 Ma)。剪切岩性大堤)具有强韧性的左侧剪切作用,这与文献中先前对垫仓山和大努伊孔伏地块的研究结果是一致的。我们还得出结论,沿ASRR剪切带的左侧剪切是印度—欧亚板块碰撞期间印度支那地块向东南挤压的结果。此外,左侧剪力还伴随着南中国海的脊突跃迁。

著录项

  • 来源
    《International Journal of Earth Sciences》 |2013年第3期|605-626|共22页
  • 作者单位

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Haidian, Beijing 100083, China,Chengdu Institute of Geology and Mineral Resources,Chengdu 610081, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Haidian, Beijing 100083, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Haidian, Beijing 100083, China,Hanoi University of Mining and Geology, Hanoi, Vietnam;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Haidian, Beijing 100083, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Haidian, Beijing 100083, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Haidian, Beijing 100083, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Haidian, Beijing 100083, China;

    Institute of Geology, Chinese Academy of Geological Sciences,Beijing 100037, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    ailao shan shear zone; granitic plutons (dykes); structural and microstructural analysis; geochronological dating; south china sea;

    机译:哀牢山剪切带花岗岩岩体(堤坝);结构和微观结构分析;年代测年南中国海;

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