Okada Y. 1992. Internal deformation due to shear and tensile faults in a half-space. Bulletin of the Seismological Society of America, 82(2): 1018-1040.
[2]
Ozawa S, Nishimura T, Suito H, et al. 2011. Coseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquake. Nature, 475(7356): 373-376.
[3]
Shi Y L, Cao J L. 2010. Some aspects in static stress change calculation—case study on Wenchuan earthquake. Chinese Journal of Geophysics (in Chinese), 53(1): 102-110, doi: 10.3969/j.issn.0001-5733.2010.01.011.
[4]
Simons M, Minson S E, Sladen A, et al. 2011. The 2011 magnitude 9.0 Tohoku-Oki earthquake: Mosaicking the megathrust from seconds to centuries. Science, 332(6036): 1421-1425.
[5]
Sun W K, Okubo S, Fu G Y, et al. 2009. General formulations of global co-eismic deformations caused by an arbitrary dislocation in a spherically symmetric earth model-applicable to deformed earth surface and space-fixed point. Geophysical Journal International, 177(3): 817-833.
[6]
Sun W K, Zhou X. 2012. Coseismic deflection change of the vertical caused by the 2011 Tohoku-Oki earthquake (Mw9.0). Geophysical Journal International, 189(2): 937-955.
[7]
Takahashi H. 2011. Static strain and stress changes in eastern Japan due to the 2011 off the Pacific coast of Tohoku Earthquake, as derived from GPS data. Earth Planets and Space, 63(7): 741-744.
[8]
Wang M, Li Q, Wang F, et al. 2011. Far-field coseismic displacements associated with the 2011 Tohoku-oki earthquake in Japan observed by Global Positioning System. Chinese Science Bulletin, 56(23): 2419-2424.
[9]
Wang R J, Martín F L, Roth F. 2003. Computation of deformation induced by earthquakes in a multi-layered elastic crust—FORTRAN programs EDGRN/EDCMP. Computers & Geosciences, 29(2): 195-207.
[10]
Yukutake Y, Honda R, Harada M, et al. 2011. Remotely-triggered seismicity in the Hakone volcano following the 2011 off the Pacific coast of Tohoku Earthquake. Earth Planets and Space, 63(7): 737-740.
[11]
Zhao B, Wang W, Yang S M, et al. 2012. Far field deformation analysis after the Mw9.0 Tohoku earthquake constrained by cGPS data. Journal of Seismology, 16(2): 305-313.
[12]
Zhu G Z, Wang Q L. 2005. Modeling of asymmetric earthquake displacement field of vertical Strike-slipe fault by using double-node finite element technique. Journal of Seismological Research (in Chinese), 28(2): 189-192.
[13]
Arnold D N. 1982. An interior penalty finite element method with discontinuous elements. SIAM Journal on Numerical Analysis, 19(4): 742-760.
[14]
Asano Y, Saito T, Ito Y, et al. 2011. Spatial distribution and focal mechanisms of aftershocks of the 2011 off the Pacific coast of Tohoku earthquake. Earth, Planets and Space, 63(7): 669-673.
[15]
Belytschko T, Black T. 1999. Elastic crack growth in finite elements with minimal remeshing. International Journal for Numerical Methods in Engineering, 45(5): 601-620.
[16]
Belytschko T, Moes N, Usui S, et al. 2001. Arbitrary discontinuities in finite elements. International Journal for Numerical Methods in Engineering, 50(4): 993-1013.
[17]
Burridge R, Knopoff L. 1964. Body force equivalents for seismic dislocations. Bulletin of the Seismological Society of America, 54(6A): 1875-1888.
[18]
Chen W T, Gan W J, Xiao G R, et al. 2012. The impact of 2011 Tohoku-oki earthquake in Japan on crustal deformation of northeastern region in China. Seismology and Geology (in Chinese), 34(3): 425-439.
[19]
Daux C, Mo？s N, Dolbow J, et al. 2000. Arbitrary branched and intersecting cracks with the extended finite element method. International Journal for Numerical Methods in Engineering, 48(12): 1741-1760.
[20]
Dolbow J, Moes N, Belytschko T. 2000. Discontinuous enrichment in finite elements with a partition of unity method. Finite Elements in Analysis and Design, 36(3-4): 235-260.
[21]
Enescu B, Aoi S, Toda S, et al. 2012. Stress perturbations and seismic response associated with the 2011 M9.0 Tohoku-oki earthquake in and around the Tokai seismic gap, central Japan. Geophysical Research Letters, 39(13), doi: 10.1029/2012GL051839.
[22]
Gonzalez-Huizar H, Velasco A A, Peng Z G, et al. 2012. Remote triggered seismicity caused by the 2011, M9.0 Tohoku-Oki, Japan earthquake. Geophysical Research Letters, 39(10), doi: 10.1029/2012GL051015.
[23]
Gracie R, Ventura G, Belytschko T. 2007. A new fast finite element method for dislocations based on interior discontinuities. International Journal for Numerical Methods in Engineering, 69(2): 423-441.
[24]
Hiratsuka S, Sato T. 2011. Alteration of stress field brought about by the occurrence of the 2011 off the Pacific coast of Tohoku earthquake (Mw9.0). Earth, Planets and Space, 63(7): 681-685.
[25]
Oden J T, Kikuchi N, Song Y J. 1982. Penalty-finite element methods for the analysis of Stokesian flows. Computer Methods in Applied Mechanics and Engineering, 31(3): 297-329.
