延边地区古洞河韧性剪切带变形特征及变形时代

张超; 刘永江; 张照录; 崔芳华; 张超; 关庆彬; 李烨

doi:10.3799/dqkx.2019.086

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3252-3264

Zhang Chao, Liu Yongjiang, Zhang Zhaolu, Cui Fanghua, Zhang Chao, Guan Qingbin, Li Ye, 2019. Deformation and Geochronological Characteristics of Gudonghe Ductile Shear Zone in Yanbian Area. Earth Science, 44(10): 3252-3264. doi: 10.3799/dqkx.2019.086

Citation:

Zhang Chao, Liu Yongjiang, Zhang Zhaolu, Cui Fanghua, Zhang Chao, Guan Qingbin, Li Ye, 2019. Deformation and Geochronological Characteristics of Gudonghe Ductile Shear Zone in Yanbian Area. Earth Science, 44(10): 3252-3264. doi: 10.3799/dqkx.2019.086

Citation:

Zhang Chao, Liu Yongjiang, Zhang Zhaolu, Cui Fanghua, Zhang Chao, Guan Qingbin, Li Ye, 2019. Deformation and Geochronological Characteristics of Gudonghe Ductile Shear Zone in Yanbian Area. Earth Science, 44(10): 3252-3264. doi: 10.3799/dqkx.2019.086

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Deformation and Geochronological Characteristics of Gudonghe Ductile Shear Zone in Yanbian Area

doi: 10.3799/dqkx.2019.086

Zhang Chao^{1,6
,},
Liu Yongjiang^2,3,4,
Zhang Zhaolu^{1
,
,},
Cui Fanghua¹,
Zhang Chao⁵,
Guan Qingbin^2,3,4,
Li Ye¹

1.
School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255049, China
2.
Key Laboratory of Submarine Geosciences and Prospecting Techniques of Ministry of Education, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3.
Institute for Advanced Ocean Study, Ocean University of China, Qingdao 266100, China
4.
Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266237, China
5.
Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
6.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources, Changchun 130061, China

Received Date: 2019-04-18
Publish Date: 2019-11-11

Abstract

Abstract

The Gudonghe ductile shear zone, located in southern section of eastern Xing-Meng orogenic belt, is a key to understanding the Late Paleozoic-Early Mesozoic tectonic evolution in Yanbian area. In this paper, zircon U-Pb dating and microstructure analysis were done for constraining the deformation time and features of Gudonghe ductile shear zone. The results show that Gudonghe ductile shear zone represents a multi-phase suite of mylonites with dextral shear thrust characteristics and W gneissosity and SW lineation. Systematic measurement of finite strains of Quartz in later mylonites indicates that the K value is 0.19 to 0.31. And Kruhl thermometer shows that the deformation temperatures of ductile shear zone range from 450 to 550℃. Fractal analysis shows that the numbers of fractal dimension vary from 1.159 to 1.214. The paleo-stress values from dynamically recrystallized grain sizes of quartz are 16.83 to 20.09 MPa, while estimated strain rates are on the order of 10^-12 to 10^-14 s^-1. The zircon U-Pb dating of granitic mylonite is 192±2 Ma, indicating that the deformation time of Gudonghe ductile shear zone is not earlier than Early Jurassic and the deformation features show the ductile shear zone thrust from southwest to northeast. However, the tectonic setting of Gudonghe ductile shear zone is mostly related to the subduction of paleo-Pacific beneath the Eurasian continent.
- Gudonghe ductile shear zone,
- fractal dimension,
- microstructure,
- Yanbian area,
- paleo-Pacific tectonic region,
- tectonics

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References(57)

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Deformation and Geochronological Characteristics of Gudonghe Ductile Shear Zone in Yanbian Area

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