Deng Q D, Chen S F, Zhao X L. 1994. Tectonics, scismisity and dynamics of Longmenshan mountains and its adjacent regions. Seismology and Geology (in Chinese), 16(4): 389-403.
[2]
Finzi Y, Langer S. 2012. Predicting rupture arrests, rupture jumps and cascading earthquakes. J. Geophys. Res., 117(B12): B12303, doi: 10.1029/2012JB009544.
[3]
Fliss S, Bhat H S, Dmowska R, et al. 2005. Fault branching and rupture directivity. J. Geophys. Res., 110(B6): B06312, doi: 10.1029/2004JB003368.
[4]
Harris R A, Day S M. 1993. Dynamics of fault interaction: parallel strike-slip faults. J. Geophys. Res., 98(B3): 4461-4472.
[5]
Harris R A, Day S M. 1999. Dynamic 3D simulations of earthquakes on en echelon faults. Geophys. Res. Lett., 26(14): 2089-2092.
[6]
Huang Y, Wu J P, Zhang T Z, et al. 2008. Relocation of the Ms8.0 Wenchuan earthquake and its after shock sequence. Science in China (Series D): Earth Sciences, 51(12): 1703-1711.
[7]
Hudnut K W, Fletcher J M, Rockwell T K, et al. 2010. Earthquake rupture complexity evidence from field observations, T51E-02. 2010 Fall Meeting. AGU, San Francisco, Calif.
[8]
Liu Z J, Sun J, Wang P, et al. 2012. Surface ruptures on the transverse Xiaoyudong fault: A significant segment boundary breached during the 2008 Wenchuan earthquake, China. Tectonophysics, 580: 218-241.
[9]
Oglesby D D, Archuleta R J, Nielsen S B. 1998. Earthquakes on dipping faults: The effects of broken symmetry. Science, 280(5366): 1055-1059.
[10]
Oglesby D D, Day S M. 2001. The effect of fault geometry on the 1999 Chi-Chi (Taiwan) earthquake. Geophys. Res. Lett., 28(9): 1831-1834.
[11]
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.
[12]
Tamura S, Ide S. 2011. Numerical study of splay faults in subduction zones: The effects of bimaterial interface and free surface. J. Geophys. Res., 116(B10), doi: 10.1029/2011JB008283.
[13]
Toda S, Stein R S, Lin J. 2011. Widespread seismicity excitation throughout central Japan following the 2011 M=9.0 Tohoku earthquake and its interpretation by Coulomb stress transfer. Geophys. Res. Lett., 38(7): L00G03, doi: 10.1029/2011GL047834.
[14]
Wesnousky S G. 2006. Predicting the endpoints of earthquake ruptures. Nature, 444(7117): 358-360.
[15]
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.
[16]
Zachariasen J, Sieh K. 1995. The transfer of slip between two en echelon strike-slip faults: A case study from the 1992 Landers earthquake, southern California. J. Geophys. Res., 100(B8): 15281-15301.
[17]
Zhang P Z, Mao F Y, Slemmons D B. 1999. Rupture terminations and size of segment boundaries from historical earthquake ruptures in the Basin and Range Province. Tectonophysics, 308(1-2): 37-52.
[18]
Zhang P Z, Xu X W, Wen X Z, et al. 2008. Slip rates and recurrence intervals of the Longmen Shan active fault zone, and tectonic implications for the mechanism of the May 12 Wenchuan earthquake, 2008, Sichuan, China. Chinese J. Geophys. (in Chinese), 51(4): 1066-1073.
[19]
Zhang Y, Feng W P, Xu L S, et al. 2009. Spatio-temporal rupture process of the 2008 great Wenchuan earthquake. Science in China (Series D): Earth Sciences, 52 (2): 145-154.
[20]
Zhang Z Q, Chen Y S, Lin J. 2008. Stress interactions between normal faults and adjacent strike-slip faults of 1997 Jiashi earthquake swarm. Science in China (Series D): Earth Sciences, 51(3): 431-440.
[21]
Zheng Y, Ma H S, Lü J, et al. 2009. Source mechanism of strong aftershocks (Ms≥5.6) of the 2008/05/12 Wenchuan earthquake and the implication for seismotectonics. Science in China (Series D): Earth Sciences, 52(6): 739-753.
[22]
Barka A A, Kadinsky-Cade K. 1998. Strike-slip fault geometry in Turkey and its influence on earthquake activity. Tectonics, 7(3): 663-684.
[23]
Chang C P, Chen G H, Xu X W, et al. 2012. Influence of the pre-existing Xiaoyudong salient in surface rupture distribution of the Mw7.9 Wenchuan earthquake, China. Tectonophysics, 530: 240-250.
[24]
Chen J H, Liu Q Y, Li S C, et al. 2009. Seismotectonic study by relocation of the Wenchuan Ms8.0 earthquake sequence. Chinese J. Geophys. (in Chinese), 52(2): 390-397.
[25]
Chen L C, Ran Y K, Wang H, et al. 2013. Paleoseismology and kinematic characteristics of the Xiaoyudong rupture, a short but significant strange segment characterized by the May 12, 2008, Mw7.9 earthquake in Sichuan, China. Tectonophysics, 584: 91-101.
[26]
Densmore A L, Ellis M A, Li Y, et al. 2007. Active tectonics of the Beichuan and Pengguan faults at the eastern margin of the Tibetan Plateau. Tectonics, 26(4): TC4005, doi: 10.1029/2006TC001987.
[27]
Duan B C, Oglesby D D. 2006. Heterogeneous fault stresses from previous earthquakes and the effect on dynamics of parallel strike-slip faults. J. Geophys. Res., 111: B05309, doi: 10.1029/2005JB004138.
[28]
Elliott A J, Dolan J F, Oglesby D D. 2009. Evidence from coseismic slip gradients for dynamic control on rupture propagation and arrest through stepovers. J. Geophys. Res., 114(B2): B02312, doi: 10.1029/2008JB005969.
[29]
Hartzell S, Mendoza C, Ramirez-Guzman L, et al. 2013. Rupture history of the 2008 Mw7.9 Wenchuan, China, Earthquake: Evaluation of separate and joint inversions of geodetic, teleseismic, and strong-motion data. Bull. Seismol. Soc. Amer., 103(1): 353-370.
[30]
Ji C, Hayes G. 2008. Preliminary result of the May 12, 2008 Mw7.9 Eastern Sichuan, China Earthquake.http://earthquakeusgsgov/ earthquakes/eqinthenews/2008/us2008ryan/finite_faultphp.
[31]
Ji C, Shao G, Lu Z, et al. 2008. Rupture history of 2008 May 12 Mw8.0 Wen-Chuan earthquake: evidence of slip interaction. EOS. Transactions of the American Geophysical Union 89 (53), S23E-02 (Fall Meet. Suppl.).
[32]
Kase Y, Kuge K. 1998. Numerical simulation of spontaneous rupture processes on two non-coplanar faults: the effect of geometry on fault interaction. Geophys. J. Int., 135(3): 911-922.
[33]
King G C P, Stein R S, Lin J. 1994. Static stress changes and the triggering of earthquakes. Bull. Seismol. Soc. Amer., 84(3): 935-953.
[34]
Li H B, Fu X F, Van der Woerd J, et al. 2008. Co-seisimic surface rupture and dextral-slip oblique thrusting of the Ms8.0 Wenchuan earthquake. Acta Geologica Sinica (in Chinese), 82(12): 1623-1643.
[35]
Liu J, Zhang Z H, Wen L, et al. 2008. The MS8.0 Wenchuanearthquake co-seismic ruptureand its tectonic implications—an out-of-sequence thrusting event with slip partitioned on multiple faults. Acta Geologica Sinica (in Chinese), 82(12): 1707-1722.
[36]
Liu Z J, Zhang Z, Wen L, et al. 2009. Co-seismic ruptures of the 12 May 2008, Ms8.0 Wenchuan earthquake, Sichuan: East-west crustal shortening on oblique, parallel thrusts along the eastern edge of Tibet. Earth Planet. Sci. Lett., 286(3-4): 355-370.
[37]
Lozos J C, Oglesby D D, Brune J N, et al. 2012. Small intermediate fault segments can either aid or hinder rupture propagation at stepovers. Geophys. Res. Lett., 39: L18305, doi: 10.1029/2012GL053005.
[38]
Magistrale H, Day S. 1999. 3D simulations of multi-segment thrust fault rupture. Geophys. Res. Lett., 26(14): 2093-2096.
[39]
Oglesby D D, Mai P M, Atakan K, et al. 2008. Dynamic models of earthquakes on the North Anatolian fault zone under the Sea of Marmara: Effect of hypocenter location. Geophys. Res. Lett., 35(18), doi: 10.1029/2008GL035037.
[40]
Okada Y. 1992. Internal deformation due to shear and tensile faults in a half-space. Bull. Seismol. Soc. Amer., 82(2): 1018-1040.
[41]
Parsons T, Stein R S, Simpson R W, et al. 1999. Stress sensitivity of fault seismicity: A comparison between limited-offset oblique and major strike-slip faults. J. Geophys. Res., 104(B9): 20183-20202.
[42]
Shao G, Ji C, Lu Z, et al. 2010. Slip history of the 2008 Mw7.9 Wenchuan earthquake constrained by jointly inverting seismic and geodetic observations. Abstract S52B-04, 2010 Fall Meeting, AGU, San Francisco.
[43]
Shen Z K, Sun J B, Zhang P Z, et al. 2009. Slip maxima at fault junctions and rupturing of barriers during the 2008 Wenchuan earthquake. Nat. Geosci, 2(10): 718-724.
[44]
Stein R S. 1999. The role of stress transfer in earthquake occurrence. Nature, 402(6762): 605-609.
[45]
Wang W M, Zhao L F, Li J, et al. 2008. Rupture process of the Ms8.0 Wenchuan earthquake of Sichuan, China. Chinese J. Geophys. (in Chinese), 51(5): 1403-1410.