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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

  • Structural Geology
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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 ºC 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 ºC. 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.

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Acknowledgments

Thanks are given to Dr. Meiling Wu for her help with mineral identification, Drs. Changcheng Li and Qihang Wu for their help with quartz c-axis fabric analysis. This work was supported by the National Natural Science Foundation of China (Nos. 41402174, 41472166), the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan), China Scholarship Council (No. 201406415007) and the Natural Sciences and Engineering Research Council of Canada. The final publication is available at Springer via https://doi.org/10.1007/s12583-017-0965-8.

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Authors and Affiliations

  1. School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China

    Xianbing Xu

  2. Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario, N2L3G1, Canada

    Xianbing Xu & Shoufa Lin

  3. School of Resources and Environment, Hefei University of Technology, Hefei, 230009, China

    Shoufa Lin

  4. No. 266 Geological Party, Nuclear Industry Geological Bureau of Jiangxi Province, Nanchang, 330013, China

    Shuai Tang

  5. State Key Laboratory for Nuclear Resources and Environment, East China Institute of Technology, Nanchang, 330013, China

    Xuefen Zhang

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  1. Xianbing Xu
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Correspondence to Xianbing Xu.

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Xu, X., Lin, S., Tang, S. et al. Transformation from Neoproterozoic Sinistral to Early Paleozoic Dextral Shearing for the Jingdezhen Ductile Shear Zone in the Jiangnan Orogen, South China. J. Earth Sci. 29, 376–390 (2018). https://doi.org/10.1007/s12583-017-0965-8

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