Slip maxima at fault junctions and rupturing of barriers during the 2008 Wenchuan earthquake

[1]  K. Hudnut,et al.  Co-seismic ruptures of the 12 May 2008, Ms 8.0 Wenchuan earthquake, Sichuan: East–west crustal shortening on oblique, parallel thrusts along the eastern edge of Tibet , 2009 .

[2]  Dong Jia,et al.  Co-seismic thrusting rupture and slip distribution produced by the 2008 Mw 7.9 Wenchuan earthquake, China , 2009 .

[3]  Hiroyuki Fujiwara,et al.  Coseismic surface‐ruptures and crustal deformations of the 2008 Wenchuan earthquake Mw7.9, China , 2009 .

[4]  Yann Klinger,et al.  Coseismic reverse- and oblique-slip surface faulting generated by the 2008 Mw 7.9 Wenchuan earthquake, China , 2009 .

[5]  J. Shaw,et al.  Uplift of the Longmen Shan and Tibetan plateau, and the 2008 Wenchuan (M = 7.9) earthquake , 2009, Nature.

[6]  E. Rogozhin,et al.  Research on Characteristics of Present‐Day Crustal Motion and Deformation in Kamchatka Area , 2009 .

[7]  ChengHu Zhou,et al.  Spatio-temporal rupture process of the 2008 great Wenchuan earthquake , 2009 .

[8]  W. Chen,et al.  Postseismic Deformation Monitoring of the 2008 Mw7.9 Wenchuan earthquake using GPS , 2008 .

[9]  Jia Cheng,et al.  GPS-constrained inversion of present-day slip rates along major faults of the Sichuan-Yunnan region, China , 2008 .

[10]  Zhao,et al.  Rupture process of the M-s 8.0 wenchuan earthquake of Sichuan, China , 2008 .

[11]  R. King,et al.  A geological and geophysical context for the Wenchuan earthquake of 12 May 2008, Sichuan, People's Republic of China , 2008 .

[12]  Peizhen Zhang,et al.  Present‐day crustal motion within the Tibetan Plateau inferred from GPS measurements , 2007 .

[13]  Michael A. Ellis,et al.  Active tectonics of the Beichuan and Pengguan faults at the eastern margin of the Tibetan Plateau , 2007 .

[14]  T. Gan,et al.  Precipitation of southwestern Canada: Wavelet, scaling, multifractal analysis, and teleconnection to climate anomalies , 2007 .

[15]  Chen Guo-guang,et al.  PRIMARY RESEARCH OF ACTIVITY SEGMENTATION OF LONGMENSHAN FAULT ZONE SINCE LATE-QUATERNARY , 2007 .

[16]  Qinglu Zeng,et al.  Longmen Shan fold-thrust belt and its relation to the western Sichuan Basin in central China: New insights from hydrocarbon exploration , 2006 .

[17]  Eth Zentrum.  GEOMORPHIC EVIDENCE FOR THE LATE CENOZOIC STRIKE-SLIPPING AND THRUSTING IN LONGMEN MOUNTAIN AT THE EASTERN MARGIN OF THE TIBETAN PLATEAU , 2006 .

[18]  Sun Hanrong,et al.  Contemporary velocity field of crustal movement of Chinese mainland from Global Positioning System measurements , 2005 .

[19]  Ma Bao-qi.  LATE QUATERNARY SLIP RATE IN THE CENTRAL PART OF THE LONGMENSHAN FAULT ZONE FROM TERRACE DEFORMATION ALONG THE MINJIANG RIVER , 2005 .

[20]  Zhi-Xun Shen,et al.  Contemporary Crustal Deformation Around Southeast Borderland of Tibetan Plateau , 2004 .

[21]  Ran Yong-kang.  LATE QUATERNARY ACTIVITY AND AGE CONSTRAINT OF THE NORTHERN LONGMENSHAN FAULT ZONE , 2004 .

[22]  Zheng‐Kang Shen,et al.  Contemporary crustal deformation of the Chinese continent and tectonic block model , 2003 .

[23]  Robert W. King,et al.  Global Positioning System measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation , 2000 .

[24]  B. Burchfiel,et al.  Tectonics of the Longmen Shan and Adjacent Regions, Central China , 1995 .