Arne D, Worley B, Wilson C, et al. 1997. Differential exhumation in response to episodic thrusting along the eastern margin of the Tibetan Plateau. Tectonophysics, 280(3-4): 239-256.
[2]
Burchfiel B C. 2004. 2003 presidential address: New technology, new geological challenges. GSA Today, 14(2): 4-9.
[3]
Burchfiel B C, Royden L H, van der Hilst R D, et al. 2008. A geological and geophysical context for the Wenchuan earthquake of 12 May 2008, Sichuan, People''s Republic of China. GSA Today, 18(7): 4-11.
[4]
Chen Z, Burchfiel B C, Liu Y, et al. 2000. Global Positioning System measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation. J. Geophys. Res., 105(B7): 16215-16227, doi: 10.1029/2000JB900092.
[5]
Clark M, Royden L H. 2000. Topographic ooze: building the eastern margin of Tibet by lower crustal flow. Geology, 28(8): 703-706.
[6]
Gan W J, Zhang P Z, Shen Z K, et al. 2007. Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements. J. Geophys. Res., 112, B08416. doi: 10.1029/2005JB004120.
[7]
Godard V, Pik R, Lavé J, et al. 2009. Late Cenozoic evolution of the central Longmen Shan, eastern Tibet: Insight from (U-Th)/He thermochronometry. Tectonics, 28, doi 10.1029/2008TC002407.
[8]
Harkins N, Kirby E, Shi X, et al. 2010. Millennial slip rates along the eastern Kunlun fault: Implications for the dynamics of intracontinental deformation in Asia. Lithosphere, 2(4): 247-266, doi: 10.1130/L85.1.
[9]
Hubbard J, Shaw J H. 2009. Uplift of the Longmen Shan and Tibetan plateau, and the 2008 Wenchuan (Ms7.9) earthquake. Nature, 458(7235): 194-197.
[10]
Hubbard J, Shaw J H, Klinger Y. 2010. Structural setting of the 2008 Mw7.9 Wenchuan, China, Earthquake. Bulletin of the Seismological Society of America, 100(5B): 2713-2735.
[11]
Li C Y, Wei Z Y, Ye J Q, et al. 2010. Amounts and styles of coseismic deformation along the northern segment of surface rupture, of the 2008 Wenchuan Mw7.9 earthquake, China. Tectonophysics, 491(1-4): 35-58.
[12]
Li Y, Huang R Q, Zhou R J, et al. 2009. Geological background of Longmen Shan Seismic Belt and surface ruptures in Wenchuan earthquake. Journal of Engineering Geology (in Chinese), 17(1): 1-10.
[13]
Li Z, Liu S, Chen H, et al. 2012. Spatial variation in Meso-Cenozoic exhumation history of the Longmen Shan thrust belt (eastern Tibetan Plateau) and the adjacent western Sichuan basin: Constraints from fission track thermochronology. Journal of Asian Earth Sciences, 47: 185-203.
[14]
Lu R Q. 2011. The geometry and kinematics of the Central Segment of the Longmenshan Mountains: Implications for the uplifting mechanism in the Southeastern Margin of Qinghai-Tibet Plateau[Ph.D.thesis] (in Chinese). Beijing:China University of Geosciences.
[15]
King R W, Shen F, Burchfiel B C, et al. 1997. Geodetic measurements of crustal motion in southwest China. Geology, 25(2): 179-182, doi: 10.1130/0091-7613.
[16]
Kirby E, Reiners P W, Krol M A, et al. 2002. Late Cenozoic evolution of the eastern margin of the Tibetan Plateau: Inferences from 40Ar/39Ar and (U-Th)/He thermochronology. Tectonics, 21(1): 1-1—1-20.
[17]
Meng Q R, Hu J M, Wang E, et al. 2006. Late Cenozoic denudation by large-magnitude landslides in the eastern edge of Tibetan Plateau. Earth and Planetary Science Letters, 243(1-2): 252-267.
[18]
Ran Y, Xu X, Chen W, et al. 2010. Paleo earthquake and large earthquakes recurrence interval along Yingxiu-Beichuan fault of the Longmenshan fault zone, Sichuan, China. Recent Developments in World Seismology (in Chinese), (6): 28-29.
[19]
Richardson N J, Densmore A L, Seward D, et al. 2008. Extraordinary denudation in the Sichuan Basin: Insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau. Journal of Geophysical Research, 113, B04409, doi: 10. 1029/2006JB004739.
[20]
Royden L H, Burchfiel B C, van der Hilst R D. 2008. The geological evolution of the Tibetan Plateau. Science, 321(5892): 1054-1058.
[21]
Shi F, He H L, Wei Z Y. 2012. Coseismic horizontal shortening associated with the 2008 Wenchuan Earthquake slong the Bashahe segment from high resolution satellite images. Journal of Asian Earth Sciences, 50: 164-170, doi: 10.1016/j. jseaes. 2012.01.001
[22]
Tan X B, Yuan R M, Xu X W, et al. 2012. Complex surface rupturing and related formation mechanisms in the Xiaoyudong area for the 2008 Mw7.9 Wenchuan Earthquake, China. Journal of Asian Earth Sciences, 58: 132-142, doi: 10.1016/j.jseaes. 2012.06.005.
[23]
Tapponnier P, Xu Z, Roger E, et al. 2001. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294(5547): 1671-1677.
[24]
Wang H, Ran Y K, Chen L C, et al. 2010. Determination of horizontal shortening and amount of reverse-faulting from trenching across the surface rupture of the 2008 Mw7.9 Wenchuan earthquake, China. Tectonophysics, 491(1): 10-20.
[25]
Xu G Q, Kamp P J J. 2000. Tectonics and denudation adjacent to the Xianshuihe Fault, eastern Tibetan Plateau: Constrains from fission track thermochronology. J. Geophys. Res., 105(B8): 19231-19251.
[26]
Xu X W, Wen X Z, Yu G H, et al. 2009. Coseismic reverse- and oblique-slip surface faulting generated by the 2008 Mw7.9 Wenchuan earthquake, China. Geology, 37(6): 515-518.
[27]
Xu X W, Chen G H, Yu G H, et al. 2010. Reevaluation of surface rupture parameters of the 5·12 Wenchuan earthquake and its tectonic implication for Tibetan uplift. Chinese J. Geophys. (in Chinese), 53(10): 2321-2336,doi:10.3969/j.issn.0001-5733.2010.10.006.
[28]
Yin A, Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan orogen. Annu. Rev. Earth Planet Sci., 28: 211-280.
[29]
Yu G, Xu X, Klinger Y, et al. 2010. Fault-Scarp features and Cascading-Ropture model for the Wenchuan earthquake (Mw7.9), Eastern Tibetan Plateau, China. Bulletin of the Seismological Society of America, 100(5B): 2590-2614. doi: 10.1785/0120090255.
