Aiming Lin,Zhiming Sun, Zhenyu Yang. 2003. Multiple generations of pseudotachylyte in the brittle to ductile regimes, Qinling Dabie Shan ultrahigh-pressure metamorphic complex, central China. The Island Arc,12(4) :423.
[27]
Christine Kumerics,Uwe Ring,Stephanie Brichau, et al. 2005. The extensional Messaria shear zone and associated brittle detachment faults, Aegean Sea, Greece. Journal of the Geological Society,162(4): 701～721.
[28]
Hanmer S. 1997. Shear zone reactivation at granulite facies: the importance of plutons in the localization of viscous flow. Journal of the Geological Society, 154 (1): 111 ～ 116.
[29]
Li J Y, Xiao W J, Wang K Z, Sun G H, Gao L M. 2003.Neoprot erozoic-Paleozoic tectonostratigraphic framework of Eastern Xinjiang, NW China. In Mao, J W, Goldfarb, R,Seltmann R, Wang D H, Xiao W J, Hart C, eds. Tectonic Evolution and Metallogeny of the Chinese Altay and Tianshan.IGCP 473 Workshop 2003, Urumuqi, International Association on the Genesis of Ore Deposits (IAGDO), CERAMS, Natural History Museum, London, 31～74.
[30]
Ludwig K R. 2001. Isoplot/Ex, rev. 2. \'49: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronological Center,Special Publication, 1: a.
[31]
Steiger R H, Jager E. 1977. Subcommission on geochronology:convention on the use of decay constants in geo- and cosmochronology. Earth Planet. Sci. Lett., 36:359～362.
[32]
Xu X W, Ma T N, Sun L Q, Cai X P. 2003. Characteristics and dynamic origin of the large-scale Jiaoluotage ductile compressional zone in the Eastern Tianshan Mountains, China. Journal of Structural Geology, 25: 1901～1915.
[33]
Xu Zhiqin. 1995. Large shear zones in the main orogenic belts of China. Episodes, 18(1～2) :41～43.
Chen Wen, Zhang Yan, Ji Qiang, Wang Songshan, Zhang Jianxin.2002. The magmatism and deformation times of the Xidatan rock series, East Kunlun Mountain. Science in China, 45( Supplement ): 20 ～ 27.
[37]
Han Chunming,Zhao Guochun. 2003. Major types and characteristics of Late Paleozoic ore deposits, East Tianshan, Northwest China.International Geology Review, 45(11): 1029～1043.
[38]
Laurent Charvet S, Charvet J, Monie P, Shu L. 2003. Late Paleozoic strike-slip shear zones in eastern central Asia (NW China): New structural and geochronological data. Tectonics, 22 (2), 1009,doi: 10. 1029/2001TC901047.
[39]
Qin Kezhang, Wang S L, Sun Su. 2001. Paleozoic epithermal Au and porphyry Cu in north Xinjiang: features, epochs and tectonic settings. International symposium on gold and hydrothermal systems, Fukuoka, Japan, 11～18.
[40]
Whitmeyer Steven J,Simpson Carol,Miro Roberto,et al. 2001. High temperature, high strain-rate fabrics define a major ductile shear zone in the eastern Sierras Pampeanas, Argentina. GSA Annual Meeting, Boston, Session, 136.
[41]
Xiao WJ, Zhang L C, Qin K Z, Sun S, Li J L. 2004. Paleozoic accretionary and collisional tectonics of the Eastern Tianshan (China): Implications for the continental growth of central Asia.American Journal of Science, 304: 370 ～ 395.
