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Lateral variation in seismic velocities and rheology beneath the Qinling-Dabie orogen

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Abstract

The Qinling-Dabie orogen is an important tectonic belt that trends east-west and divides continental China into northern and southern parts. Due to its strong deformation, complicated structure, multiphase structural superposition and the massive exposed high and ultrahigh metamorphic rocks, its tectonic formation and geodynamical evolution are hot research topics worldwide. Previous studies mainly focused on the regional geological or geochemical aspects, whereas the geophysical constraints are few and isolated, in particular on the orogenic scale. Here, we integrate the available P- and S-wave seismic and seismicity data, and construct the rheological structures along the Qinling-Dabie orogen. The results demonstrate that: (1) there are strong lateral variations in the crustal velocity between the western and eastern sections of the Qinling-Dabie orogen, indicating the different origin and tectonic evolution between these two parts; (2) the lateral variations are also manifested in the rheological structure. The rigid blocks, such as South China and Ordos basin (North China Craton), resist deformation and show low seismicity. The weak regions, such as the margin of Tibet and western Qinling-Dabie experience strong deformation and accumulated stress, thus show active seismicity; (3) in the lower crust of most of the HP/UHP terranes the values of P-wave velocity are higher than the global average ones; finally (4) low P- and S-wave velocities and low strength in the lower crust and lithospheric mantle beneath Dabie indicate lithospheric delamination, and/or high temperature, and partial melting condition.

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Acknowledgements

The paper is dedicated to the memory of Professor Zhang Zhongjie (1964–2013), who proposed the initial idea of this manuscript. Constructive comments from three anonymous reviewers have greatly improved the manuscript. We thank Dr. Qiu Zhong for valuable discussions and suggestions. We gratefully acknowledge the support offered by the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (Grant No. XDB18030101), the National Natural Science Foundation of China (Grant No. 41504069) and the Italian Projects PRIN 2010–2011, PRIN 2015.

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  1. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China

    YangFan Deng

  2. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China

    Lin Chen, Tao Xu & Jing Wu

  3. Chinese Academy of Sciences Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, China

    Tao Xu

  4. Department of Mathematics and Geosciences, University of Trieste, Via Weiss, I-34127, Trieste, Italy

    Fabio Romanelli & Giuliano Francesco Panza

  5. Institute of Geophysics, China Earthquake Administration, Beijing, 100081, China

    Giuliano Francesco Panza

  6. ISSO-International Seismic Safety Organization, Viale San Francesco, 12, I-64031, Arsita, Italy

    Giuliano Francesco Panza

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Deng, Y., Chen, L., Xu, T. et al. Lateral variation in seismic velocities and rheology beneath the Qinling-Dabie orogen. Sci. China Earth Sci. 60, 576–588 (2017). https://doi.org/10.1007/s11430-016-0101-6

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