Ratschbacher L, Hacker B, Calvert A, Webb L, Grimmer J, McWilliams M, Ireland T, Dong S and Hu J. 2003. Tectonics of the Qinling(Central China): Tectonostratigraphy, geochronology, and deformation history. Tectonophysics, 366: 1-53.
[6]
Roger F, Calassou S, Lancelot J, Malavieille J, Mattauer M, Zhiqin X, Ziwen H and Liwei H. 1995. Miocene emplacement and deformation of the Konga Shan granite(Xianshui He fault zone, west Sichuan, China): Geodynamic implications. Earth and Planetary Science Letters, 130: 201-216.
[7]
Roger F, Jolivet M, Cattin R and Malavieille J. 2011. Mesozoic-Cenozoic tectonothermal evolution of the eastern part of the Tibetan Plateau(Songpan-Garzê, Longmen Shan area): Insights from thermochronological data and simple thermal modelling. Geological Society, London, Special Publications, 353: 9.
[8]
Roger F, Leloup P H, Jolivet M, Lacassin R, Trinh P T, Brunel M and Seward D. 2000. Long and complex thermal history of the Song Chay metamorphic dome(northern Vietnam)by multi-system geochronology. Tectonophysics, 321: 449-466.
[9]
Sengr A. 1987. Tectonic subdivisions and evolution of Asia. Bull Tech Univ Istanbul, 40: 355-435.
[10]
Weislogel A, Graham S, Chang E, Wooden J, Gehrels G. and Yang H. 2006. Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks. Geology, 34: 97.
[11]
Wiedenbeck M, Alle P, Corfu F, Griffin W, Meier M, Oberli F, Quadt A, Roddick J and Spiegel W. 1995. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses. Geostandards and Geoanalytical Research, 19: 1-23.
[12]
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.
[13]
Yin H. 2003. Triassic biostratigraphy of China // Zhang W T, Chen P J and Palmer A R. Biostratigraphy of China.Beijing: Science Press: 379-422.
[14]
Yuan H, Gao S, Liu X, Li H, Günther D and Wu F. 2004. Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry. Geostandards and Geoanalytical Research, 28: 353-370.
Chang E. 2000. Geology and tectonics of the Songpan-Ganzi fold belt, southwestern China. International Geology Review, 42: 813-831.
[35]
Chew D M, Sylvester P J and Tubrett M N. 2010. U-Pb and Th-Pb dating of apatite by LA-ICPMS. Chemical Geology, 280: 200-216.
[36]
Dickinson W R. 1985. Interpreting provenance relations from detrital modes of sandstones // Zuffa G G. Provenance of arenites. Reidel Publishing Co., Dordrecht: 331-361.
[37]
Dickinson W R, Beard L S, Brakenridge G R, Erjavec J L, Ferguson R C, Inman K F, Knepp R A, Lindberg F A and Ryberg P T. 1983. Provenance of North American Phanerozoic sandstones in relation to tectonic setting. Geol Soc America Bull, 94: 222-235.
[38]
Duan L A, Meng Q R, Zhang C L and Liu X M. 2010. Tracing the position of the South China block in Gondwana: U-Pb ages and Hf isotopes of Devonian detrital zircons. Gondwana Research, 19: 141-149.
[39]
Harrowfield M and Wilson C. 2005. Indosinian deformation of the Songpan Garz fold belt, northeast Tibetan Plateau. Journal of Structural Geology, 27: 101-117.
[40]
Howard K E, Hand M, Barovich K M, Reid A, Wade B P and Belousova E A. 2009. Detrital zircon ages: Improving interpretation via Nd and Hf isotopic data. Chemical Geology, 262: 277-292.
[41]
Huang M, Buick I and Hou L. 2003. Tectonometamorphic evolution of the eastern Tibet plateau: Evidence from the central Songpan-Garze orogenic belt, western China. Journal of Petrology, 44: 255.
[42]
Miall A D. 2000. Principles of sedimentary basin analysis: Springer, New York: 66-75.
