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Hailong HUO, Da ZHANG, Zhengle CHEN, Minfeng BI, Guohua CHEN, Xiaolong HE, Ning LI, Xingjian LI, Wei XUE, Yongpeng OUYANG. DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI[J]. Journal of Geomechanics, 2018, 24(1): 9-24. doi: 10.12090/j.issn.1006-6616.2018.24.01.002
Citation: Hailong HUO, Da ZHANG, Zhengle CHEN, Minfeng BI, Guohua CHEN, Xiaolong HE, Ning LI, Xingjian LI, Wei XUE, Yongpeng OUYANG. DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI[J]. Journal of Geomechanics, 2018, 24(1): 9-24. doi: 10.12090/j.issn.1006-6616.2018.24.01.002
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DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI

  • 1.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • 2.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 3.

    Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

  • 4.

    912 Geological Team, Bureau of Geology and Mineral Resources of Jiangxi Province, Yingtan 335001, Jiangxi, China

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Received Date:  22 June 2017
Revised Date:  13 December 2017
    Abstract
  • Jingdezhen area is located in the northeastern Jiangxi province, which belongs to the Yangzi plate, and has undergone long-term tectonic activities. According to the study of regional tectonic section, the Mesozoic thrust-nappe structure direction of the study area is from NW to SE, the upper Shuangqiaoshan group has been pushed to the top of Carboniferous-Triassic strata, and the structural styles of the thrust belt are characterized by imbricate fans and duplexes and the maximum principal compressive stress is SE-NW trend. The study of undeformed granite zircon U-Pb isotope dating shows that the U-Pb isotope age is 157~172 Ma, and the time of tectonic movement is during early Yanshanian period. The Mesozoic thrust-nappe structure produced the magmatic mineralization process in the Jingdezhen area, and the granites of Jingdezhen area may have invaded from intracontinental subduction-related transformation tectonic setting during the early Yanshanian. The nappe structure constrains the magmatic evolution and in space associated with mineralization. Then it controls the mineralization process of the deposit.
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