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    Volume 32 Issue 5
    Sep.  2007
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    Article Navigation >  Earth Science  > 2007  >  32(5): 671-680
    JI Wen-hua, ZHOU Hui, LI Rong-she, CHEN Shou-jian, ZHAO Zhen-ming, 2007. The Deformation Age of Palaeozoic-Mesozoic Tectonic along North Xin-Zang Road in West Kunlun. Earth Science, 32(5): 671-680.
    Citation: JI Wen-hua, ZHOU Hui, LI Rong-she, CHEN Shou-jian, ZHAO Zhen-ming, 2007. The Deformation Age of Palaeozoic-Mesozoic Tectonic along North Xin-Zang Road in West Kunlun. Earth Science, 32(5): 671-680.
    shu

    The Deformation Age of Palaeozoic-Mesozoic Tectonic along North Xin-Zang Road in West Kunlun

    • 1.

      Xi′an Institute of Geology and Mineral Resources, Xi′an 710054, China

    • 2.

      Geological Department, Beijing University, Beijing 100871, China

    • Received Date: 2007-06-16
    • Publish Date: 2007-09-25
      Abstract
    • To establish the list of tectonic-metamorphic events in West Kunlun, we have dated tectonic metamorphic minerals such as amphibole, biotite and didrimit through 40Ar-39Ar isotopic analysis. We have gained several ages that occur many times. Combined with the emplacement age of dikes developed in this area earlier, the 440 Ma and (403±6) Ma 40Ar∕39Ar age of individual mineral biotite in gneiss can represent early Paleozoic underthrut curdle age and the period of accretional process; 382 Ma-284 Ma age of individual mineral biotite in schiefer gneiss and individual mineral amphibole in amphibolite-schist can represent the changing environment from extrusion to spread of this area in early Paleozoic era; 178 Ma-165 Ma 40Ar∕39Ar age of biotite in fragile fault can represent the spurt action of fault tectonic in the background of extrusion strike-slip tectonic and its duration.

       

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