郑亚东, Davis G A, 王琮. 2000. 燕山带中生代主要构造事件与板块构造背景问题. 地质学报, 74: 14
[31]
Brunel M, Maliakov Y. 1972. Utilisation de I′orientation preferentielle du quartz comme marqueur de la deformation hercynienne dans le granite prehercynien du Mendic (Massif Central francais). C R Acad Sci Paris, 274: 2627-2630
[32]
Davis G A, Cong W, Yadong Z, et al. 1998. The enigmatic Yinshan fold-and-thrust belt of northern China: New views on its intraplate contractional styles. Geology, 26: 43-46
[33]
Davis G A, Darby B J, Zheng Y D, et al. 2002. Geometric and temporal evolution of an extensional detachment fault, Hohhot metamorphic core complex, Inner Mongolia, China. Geology, 30: 1003-1006
[34]
Hara I, Takeda K, Kimura T. 1973. Preferred lattice orientation of quartz in shear deformation. J Sci Hiroshima Univ, 7: 1-11
[35]
Li G, Liu Z, Li S, et al. 2012. Crustal thinning during Mesozoic extensional detachment faulting in the Yiwulüshan region, eastern North China Craton. Int Geol Rev, 55: 749-766
[36]
Li S Z, Zhao G C, Sun M. 2004. Mesozoic, not Paleoproterozoic SHRIMP U-Pb zircon ages of two Liaoji Granites, eastern block, North China craton. Int Geol Rev, 46: 162-176
[37]
Li S Z, Kusky T M, Zhao G, et al. 2007. Mesozoic tectonics in the eastern block of the North China Craton: Implications for subduction of the Pacific plate beneath teh Eurasian plate. Geol Soc Spec Publ, 280: 171-188
[38]
Liu J L, Gregory A D, Lin Z Y, et al. 2005. The Liaonan metamorphic core complex, Southeastern Liaoning Province, North China: A likely contributor to Cretaceous rotation of Eastern Liaoning, Korea and contiguous areas. Tectonophysics, 407: 65-80
[39]
Liu J L, Guan H M, Ji M, et al. 2006. The Liaonan metamorphic core complex: Constitution, structure and evolution. Acta Geol Sin, 80: 502-513
[40]
Mainprice D, Bouchez J L, Blumenfeld P, et al. 1986. Dominant c slip in naturally deformed quartz: Implications for dramatic plastic softening at high temperature. Geology, 14: 819-822
[41]
Passchier C W, Trouw R A J. 1996. Microtectonics. Berlin: Springer-Verlag. 25-253
[42]
Stipp M, Stünitz H, Heilbronner R, et al. 2002. The eastern Tonale fault zone: A ‘natural laboratory'' for crystal plastic deformation of quartz over a temperature range from 250 to 700℃. J Struct Geol, 24: 1861-1884
[43]
Xiao W, Windley B F, Hao J, et al. 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt. Tectonics, 22: 1069-1088
[44]
Zhang X, Liu Q, Ma Y, et al. 2005. Geology, fluid inclusions, isotope geochemistry, and geochronology of the Paishanlou shear zone-hosted Gold Deposit, North China Craton. Ore Geol Rev, 26: 325-348
