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    Volume 46 Issue 11
    Nov.  2021
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    Article Navigation >  Earth Science  > 2021  >  46(11): 3861-3879
    Huang Liang, Wang Dongbing, Wang Xiaolin, Liu Xiaochun, Cong Feng, Zhu Xunzao, Fang Xiong, 2021. Age and Tectonic Attributes of Chongshan Group in Chongshan Metamorphic Complex in Caojian Area, West Yunnan. Earth Science, 46(11): 3861-3879. doi: 10.3799/dqkx.2020.385
    Citation: Huang Liang, Wang Dongbing, Wang Xiaolin, Liu Xiaochun, Cong Feng, Zhu Xunzao, Fang Xiong, 2021. Age and Tectonic Attributes of Chongshan Group in Chongshan Metamorphic Complex in Caojian Area, West Yunnan. Earth Science, 46(11): 3861-3879. doi: 10.3799/dqkx.2020.385
    shu

    Age and Tectonic Attributes of Chongshan Group in Chongshan Metamorphic Complex in Caojian Area, West Yunnan

    doi: 10.3799/dqkx.2020.385
    • 1.

      Yunnan Institute of Geological Survey, Kunming 650216, China

    • 2.

      MNR Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization, Kunming 650051, China

    • 3.

      Chengdu Center, China Geological Survey, Chengdu 610059, China

    • 4.

      School of Earth Sciences, Yunnan University, Kunming 650091, China

    • Received Date: 2020-12-13
      Available Online: 2021-12-04
    • Publish Date: 2021-11-30
      Abstract
    • The Chongshan metamorphic complex belt in West Yunnan is located in the northern part of "peak waist" of Sanjiang orogenic belt. The tectonic compression metamorphism in the belt is strong, and the main body is composed of a suite of medium-deep grade metamorphic rocks (Chongshan Group) and late granite.Among them, Chongshan Group has always been regarded as the crystalline basement of Proterozoic, but so far there is no accurate age basis, and its formation time and tectonic attributes are controversial, which seriously restricts the understanding of regional tectonic evolution.In this paper, the detrital zircon U-Pb geochronology and petrogeochemistry of the rock components in Chongshan Group in Caojian area, West Yunnan Province were studied. The results show that the zircons in the parametamorphic rocks have obvious rounded features and large magmatic nuclei.The smallest group of detrital zircon ages of the three samples are 366-412 Ma (mean value 395 Ma), 435-508 Ma (mean value 473 Ma) and 673-704 Ma (mean value 689 Ma), respectively, indicating that their original sedimentary age should be no earlier than 395 Ma. Rock geochemistry shows that the meta-metamorphic rocks are a set of continental island arc clastic rocks related to the tectonic setting of active continental margin or passive continental margin, and the metamorphic mafic rocks and metamorphic intermediate rocks are homologous and heterogeneous and have the characteristics of arc volcanic rocks of active continental margin.Retrogeochemistry shows that the meta-metamorphic rocks are a set of continental island arc clastic rocks related to the tectonic setting of active continental margin or passive continental margin, and the metamorphic basic rocks and metamorphic intermediate rock are homologous and heterogeneous and have the characteristics of arc volcanic rocks of active continental margin.The main body of Chongshan Group is a set of volcanic-sedimentary stratigraphic units which were diagenetic in the Late Paleozoic (236- 395 Ma) and formed in the marginal arc environment. It is combined with Silurian arc volcanic rocks of Lancang River accretion complex in the south east side to form the structural pattern of multi-island arcs in different times on the east side of the Proto- Paleo-Tethys ocean basin. According to comprehensive research, the medium-deep grade metamorphic rocks(Chongshan Group) in Chongshan metamorphic complex belt is not (all) a Proterozoic crystalline basement, but a volcanic-sedimentary stratigraphic system formed by the subduction of the original-Paleo-Tethys ocean basin eastward on the western edge of Lanping-Simao block.Chongshan Group is mainly composed of young (Late Paleozoic) stratigraphic rocks, which formed the medium-deep grade metamorphic rocks with "old" rock features after being subjected to Mesozoic and Cenozoic metamorphism and deformation in the later period.

       

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