舒兰韧性剪切带应变分析及石英动态重结晶颗粒分形特征与流变参数估算

梁琛岳; 刘永江; 孟婧瑶; 温泉波; 李伟民; 赵英利; 米晓楠; 张丽

doi:10.3799/dqkx.2015.008

Volume 40 Issue 1

Jan. 2015

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Article Navigation > Earth Science > 2015 > 40(1): 115-129

Liang Chenyue, Liu Yongjiang, Meng Jingyao, Wen Quanbo, Li Weimin, Zhao Yingli, Mi Xiaonan, Zhang Li, 2015. Strain and Fractal Analysis of Dynamically Recrystallized Quartz Grains and Rheological Parameter Estimation of Shulan Ductile Shear Zone. Earth Science, 40(1): 115-129. doi: 10.3799/dqkx.2015.008

Citation:

Liang Chenyue, Liu Yongjiang, Meng Jingyao, Wen Quanbo, Li Weimin, Zhao Yingli, Mi Xiaonan, Zhang Li, 2015. Strain and Fractal Analysis of Dynamically Recrystallized Quartz Grains and Rheological Parameter Estimation of Shulan Ductile Shear Zone. Earth Science, 40(1): 115-129. doi: 10.3799/dqkx.2015.008

Citation:

Liang Chenyue, Liu Yongjiang, Meng Jingyao, Wen Quanbo, Li Weimin, Zhao Yingli, Mi Xiaonan, Zhang Li, 2015. Strain and Fractal Analysis of Dynamically Recrystallized Quartz Grains and Rheological Parameter Estimation of Shulan Ductile Shear Zone. Earth Science, 40(1): 115-129. doi: 10.3799/dqkx.2015.008

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Strain and Fractal Analysis of Dynamically Recrystallized Quartz Grains and Rheological Parameter Estimation of Shulan Ductile Shear Zone

doi: 10.3799/dqkx.2015.008

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Department of Geology and Geography, University of Salzburg, Salzburg A-5020, Austria
3.
Boone Pickens School of Geology, Oklahoma State University, Stillwater 74078, USA
4.
Shandong Laike Engineering Design Corporation, Dongying 257000, China
5.
Shenyang Institute of Geology and Mineral Resources, Shenyang 110034, China

Received Date: 2014-05-01
Publish Date: 2015-01-15

Abstract

Abstract

Shulan ductile shear zone represents a suit of mylonites with sinistral strike-slip characteristics and NNE gneissosity located in south-middle part of the Jiamusi-Yitong fault (called Jia-Yi fault in short). Systematic measurement of the finite strains of feldspar in mylonites indicates that the strain type is extension strain in L-S tectonites. Quartz C-axis EBSD fabric indicates that the quartz fabrics is mainly low-middle temperature prism-glide fabrics with slip system of {0001} < 110>. By calculation of micro structures and quartz C-axis fabrics, it is found that the shearing strain is 0.44; all kinematic vorticities are all more than 0.95, which indicates that the deformation is mainly simple shear. Mineral deformation behaviors, quartz C-axis EBSD fabrics, quartz grain size-frequency diagram and Kruhl thermometer demonstrate that the ductile shear zone was developed under a condition of low-grade greenschist facies, with deformation temperatures ranging from 400 to 500 ℃, and dislocation creep is the main deformation mechanism. The shapes of recrystallized quartz grains in mylonites with their jagged and indented boundaries are natural records of deformation conditions. Fractal analysis shows that the boundaries of recrystallized grains have statistically self-similarities with the numbers of fractal dimension from 1.195 to 1.220. The paleo-stress from dynamically recrystallized grain sizes of quartz are 24.35-27.59 MPa, representing the lower limit of the paleo-stress during mylonization. Together with temperature estimates and applying published flow laws, it is concluded that estimated strain rates on the order of 10^-12.00 to 10^-13.18 s^-1, contrasting with regional strain rate of 10^-13.00 to 10^-15.00 s^-1, indicate deformation of mylonite in Shulan ductile shear zone with low strain rates which are consistent with most other ductile zone, suggest the deformation is slow process. Taking into consideration of the regional tectonic setting of NE China, we suggest that the formation of the ductile shear zone with NNE trending might be related to moving direction changing of the Izanagi plate obliquely subducting under the Eurasia plate.
- Shulan ductile shear zone,
- quzrtz dynamic recrystallization,
- finite-strain determination,
- kinematic vorticity,
- fractal dimension,
- differential stress,
- strain rate,
- Jia-Yi fault,
- structural geology

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References(107)

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Strain and Fractal Analysis of Dynamically Recrystallized Quartz Grains and Rheological Parameter Estimation of Shulan Ductile Shear Zone

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