Late Mesozoic and Cenozoic thermotectonic evolution along a transect from the north China craton through the Qinling orogen into the Yangtze craton, central China
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چکیده
, Earth Sci. Frontiers, 12(2), 247–262.Xu, C., Z. Zhou, P. Van Den Haute, R. A. Donelick,J. De Grave, M. A. Changqian, and P. W. Reiners (2005), Apatite fission track geochronology and itstectonic correlation in the Dabieshan orogen,central China, Sci. China, Ser. D, 48, 506–520.Xue, F., A. Kröner, T. Reischmann, and F. Lerch(1996a), Palaeozoic preand post-collision calc-alkaline magmatism in the Qinling orogenic belt, cen-tral China, as documented by zircon ages ongranitoid rocks, J. Geol. Soc., 153, 409 –417. Xue, F., F. Lerch, A. Kröner, and T. Reischmann (1996b),Tectonic evolution of the East Qinling Mountains,China, in the Paleozoic: A review and a new tectonicmodel, Tectonophysics, 253, 271–284. Yin, A., and T. M. Harrison (2000), Geological Evolu-tion of the Himalayan–Tibetan orogen, Annu. Rev.Earth Planet. Sci., 28, 211–280. Yin, A., and S. Nie (1996), A Phanerozoic palinspasticreconstruction of China and its neighboring regions,in The Tectonic Evolution of Asia, edited by A. Yinand T. M. Harrison, pp. 442–485,Cambridge Univ. Press, New York.Yin, G., Y. Lu, H. Zhao, W. Li, L. Li, and S. Guo(2001), The tectonic uplift of the Hua Shan in the Cenozoic, Chinese Sci. Bull., 46, 1665–1668.Zhai, X., H. W. Day, B. R. Hacker, and Z. You (1998),Paleozoic metamorphism in the Qinling orogen,Tongbai Mountains, central China, Geology, 26, 371 –374.Zhang, G., Z. Yu, Y. Sun, S. Cheng, T. Li, F. Xue, andC. Zhang (1989), The major suture zone of the Qinling orogenic belt, J. Southeast Asian EarthSci., 3, 63– 76.Zhang, Y. Q., P. Vergely, and J. L. Mercier (1995),Active faulting in and along the Qinling Range (China) inferred from SPOT imagery analysis andextrusion tectonics of southern China, Tectonophy-sics, 243, 69– 95. Zhang, Y. Q., J. L. Mercier, and P. Vergeley (1998),Extension in the graben system around the Ordos(China), and its contribution to the extrusion tec-tonics of south China with respect to Gobi-Mongolia, Tectonophysics, 285, 41 –75.Zhang, Y. Q., P. Vergely, J. L. Mercier, Y. Wang,Y. Zhang, and D. Huang (1999), Kinematic history and changes in the tectonic stress regime during theCenozoic along the Qinling and southern Tanlufault zones, Acta Geol. Sin., 73, 264–274.Zhang, Z. (1996), Eclogite-facies metamorphism in the amphibolites in the contact with mantle peridotite inthe Proterozoic Songshugou ophiolite complex,Qinling mountains, China, Eos Trans. AGU, 77(46), Fall Meet. Suppl., F766.Zhang, Z., G. Zhang, S. Tang, and J. Wang (2001), Onthe age of metamorphic rocks of the Yudongzigroup and Archean crystalline basement of the Qinling orogen, Acta Geol. Sin., 75, 198–204.Zhang, Z. Q., D. Y. Liu, and G. M. Fu (1991) Ages ofthe Qinling, Kuanping, and Taowan groups in theNorth Qinling orogenic belt, middle China and their implications, in A Selection of Papers Presented atthe Conference on the Qinling Orogenic Belt, editedby L. J. Ye, X. L. Qian, and G. W. Zhang, pp. 214– 228, Northwest Univ. Press, Xi’an, China.Zhou, Z., C. Xu, P. W. Reiners, F. Yang, and R. A.Donelick (2003), Late Cretaceous-Cenozoic exhu-mation history of Tiantangzhai region of Dabieshan orogen: Constraints from (U-Th)/He and fission-track analysis, Chin. Sci. Bull., 48, 1151 –1156. A. J. W. Gleadow, B. P. Kohn, and A. Raza, Schoolof Earth Sciences, University of Melbourne, Melbourne
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Creation and Destruction of Lithospheric Mantle beneath the North China Craton
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