安徽省休宁—歙县整装勘查区晚侏罗世逆冲推覆构造特征及其与成矿作用关系

doi:10.13278/j.cnki.jjuese.20190310

Abstract

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

Weng Wangfei, Wang Deen, Hu Zhaoqi, Zhu Qiang, Wang Qinian, Wu Jiming, Tang Guoqiang, Zhang Pengfei. Characteristics of Thrust-Nappe Structure and Its Relationship with Mineralization in Xiuning-Shexian Integrated Exploration Area, Anhui Province[J].Journal of Jilin University(Earth Science Edition), 2020, 50(5): 1518-1538.

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

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