Brookfield M E. 1998. The evolution of the great river systems of southern Asia during the Cenozoic India-Asia collision: Rivers draining southwards. Geomorphology, 22: 285-312
[13]
Bruguier O, Lancelot J R, Malavieille J. 1997. U-Pb dating on single detrital zircon granites from the Triassic Songpan-Ganzi flysch (Central China): Provenance and tectonic correlations. Earth Planet Sci Lett, 152: 217-231
[14]
Chappell J, Zheng H, Fifield K. 2006. Yangtse River sediments and erosion rates from source to sink traced with cosmogenic 10Be: Sediments from major rivers. Palaeogeog Palaeoclimatol Palaeoecol, 241: 79-94
[15]
Dunai T J. 2010. Cosmogenic Nuclides: Principles, Concenpts and Applications in the Earth Surface Sciences. Cambridge: Cambridge University Press. 187
[16]
Enkelmann E, Weislogel A, Ratschbacher L, et al. 2007. How was the Triassic Songpan-Ganzi basin filled? A provenance study. Tectonics, 26: TC4007, doi: 10.1029/2006TC002078
[17]
Kong P, Zheng Y, Caffee M C. 2012. Provenance and time constraints on the formation of the first bend of the Yangtze River. Geochem Geophys Geosyst, 13: Q06017, doi: 10.1029/2012GC004140
[18]
Leloup P H, Harrison T M, Ryerson F J, et al. 1993. Structural, petrological and thermal evolution of a Tertiary ductile strike-slip shear zone, Diancang Shan, Yunnan. J Geophys Res, 98: 6715-6743
[19]
Leloup P H, Lacassin R, Tapponnier P, et al. 1995. The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina. Tectonophysics, 251: 3-84
[20]
Li S, Deng C, Yao H, et al. 2013. Magnetostratigraphy of the Dali Basin in Yunnan and implications for Late Neogene rotation of the southeast margin of the Tibetan Plateau. J Geophys Res, 118: 791-807
[21]
Molnar P, Tapponnier P. 1975. Cenozoic tectonics of Asia: Effects of a continental collision. Science, 189: 419-426
[22]
Nishiizumi K, Lal D, Klein J,et al. 1986. Production of 10Be and 26Al by cosmic rays in terrestrial quartz in situ and implications for erosion rates. Nature, 319: 134-136
[23]
Sun B N, Wu J Y, Liu Y S, et al. 2011. Reconstructing Neogene vegetation and climates to infer tectonic uplift in western Yunnan, China. Palaeogeog Palaeoclim Palaeoecol, 304: 328-336
[24]
Tapponnier P, Lacassin R, Leloup P H, et al. 1990. The Ailao Shan/Red River metamorphic belt: Tertiary left-lateral shear between Indochina and South China. Nature, 343: 431-437
[25]
Wang E, Burchfiel B C. 2000. Late Cenozoic to Holocene deformation in southwestern Sichuan and adjacent Yunnan, China, and its role in formation of the southeastern part of the Tibetan Plateau. Geol Soc Am Bull, 112: 413-423
[26]
Wang E, Burchfiel B C, Royden L H, et al. 1998. Late Cenozoic Xianshuihe-Xiaojiang, Red River, and Dali fault systems of southwestern Sichuan and central Yunnan, China. Geol Soc Am Spec Paper. 327: 1-108
[27]
Yin A, Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan orogen. Ann Rev Earth Planet Sci, 28: 211-280
[28]
Fan C, Wang G, Wang S, et al. 2006. Structural interpretation of extensional deformation along the Dali fault system, southeastern margin of the Tibetan Plateau. Int Geol Rev, 48: 287-310
[29]
Gosse J C, Phillips F M. 2001. Terristrial in situ cosmogenic nuclides: Theory and application. Quat Sci Rev, 20: 1475-1560
[30]
Granger D E, Kirchner J W, Finkel R C, et al. 1997. Quaternary downcutting rate of the New River, Virginia, measured from different decay of cosmogenic 26Al and 10Be in cave-deposited alluvium. Geology, 25: 107-110
[31]
Granger D E, Muzikar P F. 2001. Dating sediment burial with in situ-produced cosmogenic nuclides: Theory, techniques, and limitations. Earth Planet Sci Lett, 188: 269-281
[32]
Kong P, Granger D, Wu F Y, et al. 2009. Cosmogenic nuclide burial ages and provenance of the Xigeda paleo-lake: Implications for evolution of the Middle Yangtze River. Earth planet Sci Lett, 278: 131-141
[33]
Kong P, Zheng Y, Fu B. 2011. Cosmogenic nuclide burial ages and provenance of Late Cenozoic deposits in the Sichuan Basin: Implications for Early Quaternary glaciations in east Tibet. Quat Geochron, 6: 304-312