Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (3): 769-783.doi: 10.13278/j.cnki.jjuese.20170194

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Zircon U-Pb Ages and Its Geological Implication of Mesozoic Granites in Tuquan-Keerqin Youyizhongqi Region

Gao Fei1,2, Liu Yongjiang1,2, Wen Quanbo1, Li Weimin1, Feng Zhiqiang3, Fan Wenliang4, Tang Chao5   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources of China, Changchun 130061, China;
    3. College of Mining Engineering, Taiyuan University of Technology, Taiyuan 030024, China;
    4. Changchun Gold Research Institute, Changchun 130012, China;
    5. Laboratory of Non-fossil Energy Minerals, Tianjin Center of China Geological Survey, Tianjin 300170, China
  • Received:2017-09-17 Online:2018-05-26 Published:2018-05-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41230206,41102140,41602235) and Project Tianjin Center of China Geological Survey(DD20160128-04)

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Abstract: Tuquan-Keerqin Youyizhongqi of Inner Mongolia is located in the central and southern Da Hinggan Range, where the Mesozoic magmatic activity was frequent. The rocks are mainly composed of granodiorite, syenite, monzonitic granite, and granite porphyry etc. We studied the Mesozoic granites in the whole area to obtain the related geological data,tested the LA-ICP-MS zircon U-Pb age,divided the different Mesozoic magmatism periods on the basis of the predecessors' data,and then discussed the geological significance of the different granites in this area. Several samples of the three magmatic intrusive rocks from this region were dated by the LA-ICP-MS technique. The result indicates that the granodiorite of Mengentaolegai pluton was emplaced at (241.2±2.8) Ma, the syenite in the southern Duerji was emplaced at (148.2±1.0) Ma, the monzonitic granite of Baogetu pluton was emplaced at (226.0±1.1) Ma, and the granite porphyry of the Majiatun pluton was emplaced at (124.6±1.1) Ma, corresponding to the ages of the volcanic rocks respectively. Combining with the previous and adjacent geological data, we divided the magmatic activity into three periods:Middle-Late Triassic, Late Jurassic, and Early Cretaceous. We conclude that the Middle-Late Triassic granites may be the product of the post-orogenic lithospheric extension of the Paleo-Asian Ocean closure, and the formation of the Late Jurassic granites may be related to the Mongol-Okhotsk Ocean closure; while the Early Cretaceous granites might reflect the extensional tectonic setting.

Key words: Da Hinggan Range, Tuquan-Keerqin Youyizhongqi area, Mesozoic, granite, zircon U-Pb age

CLC Number: 

  • P588.1
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