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Palaeozoic tectonics of the south-western Chinese Tianshan: new insights from a structural study of the high-pressure/low-temperature metamorphic belt

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Abstract

The south-western Chinese Tianshan orogenic belt is famous for its omphacite-bearing blueschists and associated eclogite-facies metavolcanic rocks. Although numerous petrologic, geochemical and geochronological studies are available, structural data and interpretations are still rare. This paper provides new structural data, including bulk geometry of structures and kinematic analyses, based on field and laboratory studies along the Akyazhi, Keburt and Muzaert Rivers. The study area is divided into three tectonic units, namely (1) a Southern Unit composed of weakly metamorphosed sedimentary rocks of Silurian age; (2) a Central HP/LT Unit composed of blueschist-eclogite-facies metamorphic rocks derived from basalts, pelites and volcaniclastic rocks; (3) a Northern Unit, which consists of a Carboniferous magmatic arc developed upon an amphibolite-facies metamorphic continental basement. Our structural analysis documents a polyphase deformation. The main event (D1) is reflected by Devonian to Carboniferous top-to-the northwest ductile shearing, coeval with HP/LT metamorphism. This is followed by north-directed thrusting (D2) of the Southern Unit over the Central HP/LT Unit, coeval with retrogression of the high-pressure rocks. A top-to-the-S (SE) deformation (D3) overprints the earliest events and is observed in the Northern and Central Units. Lastly, Permian dextral ductile-brittle wrenching (D4) overprints the older flat-lying fabrics. D4 is conspicuous along the Nalati Fault that separates the Northern Unit from the Central HP/LT Unit. The absolute timing of these deformation events is discussed in the light of available radiometric dating. The structural, metamorphic and geochronological data are integrated into a geodynamic model of the south-western Chinese Tianshan that emphasizes south-directed subduction of microcontinents located between Tarim and Junggar.

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Acknowledgments

W. Lin expresses his sincere thanks to J. Gao for discussions and useful information (especially photos in Figs. 6b–d). Constructive comments on science and English by J. Charvet, L. F. Zhang and D. Alexeiev are deeply acknowledged. We also thank Alfred Kroener for his helpful editorial advice. Field and laboratory work were supported by Chinese National 973 Project no. 2009CB825008 and NSFC grant (40472069).

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  1. SKL, Institute of Geology and Geophysics, Chinese Academy of Sciences, P. O. Box 9825, Beijing, 100029, China

    Wei Lin, Qingchen Wang & Zhong Li

  2. ISTO, UMR-CNRS 6113, Université d’Orléans, 45067, Orléans Cedex 2, France

    Michel Faure

  3. Department of Geology, School of Resource and Environment Engineering, Hefei University of Technology, Tunxi Road 193, Hefei, Anhui, 230009, China

    Yonghong Shi

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Correspondence to Wei Lin.

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Submitted to, Thematic volume on Geodynamic Evolution of Central Asia in the Palaeozoic and Mesozoic in International Journal of Earth Sciences .

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Lin, W., Faure, M., Shi, Y. et al. Palaeozoic tectonics of the south-western Chinese Tianshan: new insights from a structural study of the high-pressure/low-temperature metamorphic belt. Int J Earth Sci (Geol Rundsch) 98, 1259–1274 (2009). https://doi.org/10.1007/s00531-008-0371-7

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