Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (5): 1518-1538.doi: 10.13278/j.cnki.jjuese.20190310

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Characteristics of Thrust-Nappe Structure and Its Relationship with Mineralization in Xiuning-Shexian Integrated Exploration Area, Anhui Province

Weng Wangfei1, Wang Deen1, Hu Zhaoqi2, Zhu Qiang2, Wang Qinian3, Wu Jiming1, Tang Guoqiang1, Zhang Pengfei1   

  1. 1. 332 Geological Team, Bureau of Geology and Mineral Resources Exploration of Anhui Province, Huangshan 245000, Anhui, China;
    2. Geological Survey of Anhui Province, Hefei 230001, China;
    3. Geological Exploration Technology Institute of Anhui Province, Hefei 230041, China
  • Received:2019-12-25 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by Project of China Geological Survey (12120114028501, 121201004000150017-4, 121201004000160901-11, 121201004000160901-09, DD20190159-20),Commonweal Geological Project of Anhui Province(2014-g-1) and Science and Technology Project of Anhui Province (2014-K-1)

Abstract: Based on the field geological survey and the comprehensive tectonic interpretation of magnetotelluric sounding electromagnetic array profile, a large-scale thrust-nappe structure is developed in the Late Jurassic in the integrated gold polymetallic ore exploration area in Xiuning-Shexian and its adjacent area, which consists of thrust fault, thrust sheet, original rock series, structural window,and associated traction fold. The thrust-nappe structure is developed in the southern edge of "Tunxi-Xiuning" Mesozoic continental sedimentary basin, which shows that the Neoproterozoic shallow metamorphosed volcano clastic rock series is thrust napped on the clastic rock of Hongqin Formation in Middle Jurassic. The thrust-nappe structure is composed of a series of branch thrust faults, which are characterized by the pre-spreading imbricate thrust. The front edge of the fault is steep and becomes gentle downward. The thrust-nappe structure is distributed in the northeast direction extending up to 40 km in the area, and the nappe area is more than 600 km2 in the integrated exploration area. According to the exposed position of the structural window and combined with drilling and geophysical exploration, the thrust displacement is 2.0-8.0 km. According to the time-space matching of thrust faults,the sedimentary strata,and magmatic activity, it is estimated that the formation time of the Late Jurassic thrust-nappe structure is 163.5-149.0 Ma. Based on the observation of the friction marks of the thrust faults and the analysis of the paleo-stress field, it is believed that the thrust-nappe structure was formed in the regional dynamic environment of the strong northward compression of the South China plate. The thrust-nappe structure is a pre metallogenic structure, its and the later extensional structures play an important role in the intrusion of magma and the circulation of ore-bearing hydrothermal fluid. The thrust-nappe structure controls the distribution and enrichment of gold, silver, lead-zinc, and other low-temperature elements in the integrated exploration area.

Key words: thrust-nappe structure, magnetotelluric sounding electromagnetic array profile, mineralization, Yanshanian, integrated exploration area, Xiuning-Shexian

CLC Number: 

  • P542
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