13th International Conference on Fracture June 16–21, 2013, Beijing, China -11- Fig.5 Yinxiu fault and Pengxian fault in Wenchuan Earthquake Acknowledgements The work was supported by National Natural Science Foundation of China (NOD0408/4097409), Chairmen Foundation of UCAS [A](D0408/4097409) and Deep exploration in China-Sinoprobe-04 (0819011A90). References [1] Zhang W Y,Introduction to Faulting Blocks, Beijing, Petro Industry Press, 1984 (in Chinese). [2] Ma Jin, Transition from fault theory to block theory on China strong earthquakes, Earth Science Front, 1999, 6, 33-370 (in Chinese). [3] Ma Xin Yuan, Dynamics Figures of China Lithosphere, Beijing, Geography Press, 1989 (in Chinese). [4]Ding Guo Yu, Introduction to China Lithosphere Dynamics,Seismological Press, 1991(in Chinese). [5] Ma S L, Annual Spectrum of Professor Li Shi Guang, Beijing,Geological Press, 1989 (in Chinese) [6] Maruyama T, Fan T Y，A breakdown zone model of a fault in a strip, J Phys Earth, 1993,41, 21-39. [7] Fan T Y, Exact solution of semi-infinite crack in a strip, Chin PhysLett, 1991, 7, 402-404. [8] Shen D W and Fan T Y,Exact solutions of two semi-infinite cracks in a strip, Eng Fract Mech, 2003, 70, 813-822. [9] Fan T Y, Fracture Dynamics—Principle and Applications, 2006, Beijing, Beijing Institute of Technology (in Chinese). [10] Sun Z F, Fan T Y, Tectonic stress field of Ms 8.0 Wenchuan earthquake of May 8, 2008, J Beijing Inst Tech, 2010, 30, 253-257. [11] Tada H, Paris P C, Irwin G R, The Stress Analysis of Cracks Handbook, Del Research Cooperation, Hellertown,1973.
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