Lin J L, Fuller M and Zhang W Y. 1985. Preliminary Phanerozoic polar wander paths for the North and South China Blocks. Nature, 313: 444?449.
[2]
Liu S F, Steel R and Zhang G W. 2005. Mesozoic sedimentary basin development and tectonic implication, northern Yangtze Block, eastern China: Record of continent-continent collision. Journal of Asian Earth Sciences, 25: 9?27.
[3]
Macedo C and Marshak S. 1999. Controls on the geometry of fold-thrust belt salients. Geological Society of America Bulletin, 111(12): 1808?1822.
[4]
Meng Q R, Wang E C and Hu J M. 2005. Mesozoic sedimentary evolution of the northwest Sichuan basin: Implication for continued clockwise rotation of the South China block. Geological Society of America Bulletin, 117: 396?410.
[5]
Meng Q R and Zhang G W. 2000. Geologic Framework and Tectonic Evolution of the Qin ling Orogen, Central China. Tectonophysics, 323(3/4): 183?196.
[6]
Okay A I and Sengor A M C. 1992. Evidence for intracontinental thrust-related exhumation of the ultrahigh-pressure rocks in China. Geology, 20: 411?414.
[7]
Zhang G W, Meng Q R, Yu Z P, Sun Y, Zhou D W and Guo A L. 1996. Orogenesis and dynamics of the Qinling orogen. Science in China (Series D), 39: 225?234.
[8]
Zhao X X and Coe R S. 1987. Paleomagnetic constraints on the collision and rotation of North and South China. Nature, 327: 141?144.
Dong S W, Gao R, Yin A, Guo T L, Zhang Y Q, Hu J M, Li J H, Shi W and Li Q S. 2013. What drove continued continent-continent convergence after ocean closure? Insights from high-resolution seismic-reflection profiling across the Daba Shan in central China. Geology, 41(6): 671?674.
[29]
Eide E A. 1993. Petrology, Geochronology, and Structure of High-pressure Metamorphic Rocks in Hubei Province, East-central China, and Their Relationship to Continental Collision. Ph. D. dissertation, Stanford University: 1?470.
[30]
Enkin R J, Yang Z, Chen Y and Courtillot V. 1992. Paleomagnetic constraints on the geodynamic history of the major blocks of China from Permian to the present. Journal of Geophysical Research, 97: 13953?13989.
[31]
Gilder S and Courtillot V. 1997. Timing of the North?South China collision from new Middle to Late Mesozoic paleomagnetic data from the North China Block. Journal of Geophysical Research, 102: 17713?17727.
[32]
Gilder S A, Leloup P H, Courtillot V, Chen Y, Coe R S, Zhao X, Xiao W, Halim N, Cogne J P and Zhu R. 1999. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via Middle Triassic to Early Cenozoic paleomagnetic data. Journal of Geophysical Research, 104(B7): 15365?15390.
[33]
Hu J M, Chen H, Qu H J, Wu G L, Yang J X and Zhang Z Y. 2012. Mesozoic deformations of the Dabashan in the southern Qinling orogen, central China. Journal of Asian Earth Sciences, 47: 171?184.
[34]
Huang K N and Opdyke N D. 1991. Paleomagnetism of Jurassic rocks from southwestern Sichuan and the timing of the closure of the Qinling suture. Tectonophysics, 200: 299?316.
[35]
Nie S, Yin A, Rowley D B and Jin Y. 1994. Exhumation of the Dabie Shan ultra-high-pressure rocks and accumulation of the Songpan Ganze flysch sequence, central China. Geology, 22: 999?1002.
[36]
Sengor A M C, Gorur N and Saroglu F. 1985. Strike-slip faulting and related basin formation in zones of tectonic escape: Turkey as a case study // Biddle K T and Christe-Blick N. Strike-slip deformation, basin formation and sedimentation. Society Economic Paleontologist and Mineralogists, Special Publication, 37: 227?265.
[37]
Shi W, Zhang Y Q, Dong S W, Hu J M, Wiesinger M, Ratschbacher L, Jonckheere R, Li J H, Tian M, Chen H, Wu G L, Ma L C and Li H L. 2012. Intra-continental Dabashan orocline, southwestern Qinling, Central China. Journal of Asian Earth Sciences, 46(2): 20?38.
[38]
Tan X D, Kodama K P, Gilder S, Courtillot V and Cogne J P. 2007. Paleomagnetic evidence and tectonic origin of clockwise rotations in the Yangtze fold belt, South China Block. Geophysical Journal International, 168: 48?58.
[39]
Wang E, Meng Q R, Burchfiel B C and Zhang G W. 2003. Mesozoic large-scale lateral extrusion, rotation, and uplift of the Tongbai-Dabie Shan belt in east China. Geology, 31(4): 307?310.
[40]
Yang Z Y, Courtillot V, Besse J, Ma X H, Xing L S, Xu S J and Zhang J X. 1992. Jurassic paleomagnetic constraints on the collision of the North and South China Blocks. Geophysical Research Letters, 19: 577?580.
[41]
Yin A and Nie S. 1993. An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems, eastern Asia. Tectonics, 12: 801?813.
[42]
Yokoyama M, Liu Y Y, Halim N and Otofuji Y. 2001. Paleomagnetic study of Upper Jurassic rocks from the Sichuan basin: Tectonic aspects for the collision between the Yangtze Block and the North China Block. Earth and Planetary Science Letters, 193: 273?285.
[43]
Zhang H, Tan X D and Han Y L. 2007. Cretaceous synfolding remagnetization components revealing tectonic rotation of the middle Yangtze fold belt. Chinese Science Bulletin, 52(20): 2837?2846.
[44]
Zhang K J. 2002. Escape hypothesis for the North and South China collision and the tectonic evolution of the Qinling orogen, eastern Asia. Eclogae Geologicae Helvetiae, 95: 237?247.
[45]
Zhu G, Liu G S, Niu M L, Xie C L, Wang Y S and Xiang B W. 2009. Syn-collisional transform faulting of the Tan-Lu fault zone, East China. International Journal of Earth Sciences, 98(1): 135?155.