Transformation from Neoproterozoic Sinistral to Early Paleozoic Dextral Shearing for the Jingdezhen Ductile Shear Zone in the Jiangnan Orogen, South China

Xianbing Xu; Shoufa Lin; Shuai Tang; Xuefen Zhang

doi:10.1007/s12583-017-0965-8

Volume 29 Issue 2

Mar 2018

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Journal of Earth Science > 2018 > 29(2): 376-390.

Xianbing Xu, Shoufa Lin, Shuai Tang, Xuefen Zhang. Transformation from Neoproterozoic Sinistral to Early Paleozoic Dextral Shearing for the Jingdezhen Ductile Shear Zone in the Jiangnan Orogen, South China. Journal of Earth Science, 2018, 29(2): 376-390. doi: 10.1007/s12583-017-0965-8

Citation:

Xianbing Xu, Shoufa Lin, Shuai Tang, Xuefen Zhang. Transformation from Neoproterozoic Sinistral to Early Paleozoic Dextral Shearing for the Jingdezhen Ductile Shear Zone in the Jiangnan Orogen, South China. Journal of Earth Science, 2018, 29(2): 376-390. doi: 10.1007/s12583-017-0965-8

Citation:

Xianbing Xu, Shoufa Lin, Shuai Tang, Xuefen Zhang. Transformation from Neoproterozoic Sinistral to Early Paleozoic Dextral Shearing for the Jingdezhen Ductile Shear Zone in the Jiangnan Orogen, South China. Journal of Earth Science, 2018, 29(2): 376-390. doi: 10.1007/s12583-017-0965-8

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Transformation from Neoproterozoic Sinistral to Early Paleozoic Dextral Shearing for the Jingdezhen Ductile Shear Zone in the Jiangnan Orogen, South China

doi: 10.1007/s12583-017-0965-8

Xianbing Xu^{1,2
,
,},
Shoufa Lin^2,3,
Shuai Tang⁴,
Xuefen Zhang⁵

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario N2L3G1, Canada
3.
School of Resources and Environment, Hefei University of Technology, Hefei 230009, China
4.
No. 266 Geological Party, Nuclear Industry Geological Bureau of Jiangxi Province, Nanchang 330013, China
5.
State Key Laboratory for Nuclear Resources and Environment, East China Institute of Technology, Nanchang 330013, China

More Information

Corresponding author: Xianbing Xu, xbxu2011@cug.edu.cn
Received Date: 12 Oct 2017
Accepted Date: 25 Nov 2017
Publish Date: 01 Feb 2018

Abstract

Abstract

The Jingdezhen ductile shear zone is evolved from the Neoproterozoic Zhangyuan ophiolite mélange belt in the eastern Jiangnan Orogen, South China. Comprehensive study of geometry, kinematics, quartz c-axis fabric, temperature-pressure conditions and geochronology were conducted in this study. The Jingdezhen shear zone extends ~180 km along the NE orientation with two groups of subvertical foliation and subhorizontal lineation. One group of foliation strikes NEN orientation whereas another one NEE orientation. Field investigation, microscopic observation and quartz c-axis fabric show that sinistral shearing along NEN-striking foliation occurred earlier than dextral shearing along NEE-striking foliation. Syn-tectonic staurolite porphyroblasts and deformation manner of feldspar imply that sinistral shearing occurred at 530–420 C and 6–2 kbar. Deformation manner and c-axis fabric of quartz and pre-tectonic staurolite porphyroblasts indicate that dextral shearing took place at 420–300 C. LA-ICP-MS zircon U-Pb and mica ⁴⁰Ar/³⁹Ar dating indicate that the sinistral shearing occurred during Neoproterozoic orogeny (830–800 Ma) whereas the dextral shearing at 447±12 Ma. The sinistral shearing resulted from the Neoproterozoic final assembly between the Yangtze and Cathaysia blocks. The dextral shearing was caused by Early Paleozoic orogen parallel extension and clockwise rotation.
- Jingdezhen ductile shear zone,
- quartz c-axis fabric,
- temperature-pressure condition,
- geochronology,
- Jiangnan Orogen,
- South China

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References(98)

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