Crampin S, Booth D C. Shear-wave polarizations near the North Anatolian Fault-II, Interpretation in terms of crack-induced anisotropy. Geophys. J. R Astron. Soc., 1985, 83(1): 75-92.
[2]
Schoenberg M. Elastic wave behavior across linear slip interfaces. Journal of the Acoustical Society of America, 1980, 68(5): 1516-1521.
[3]
Schoenberg M, Douma J. Elastic wave propagation in media with parallel fractures and aligned cracks. Geophys. Prospect., 1988, 36(6): 571-590.
[4]
Hudson J A. Wave speeds and attenuation of elastic waves in material containing cracks. Geophys. J. Int., 1981, 64(1): 133-150.
[5]
Hudson J A, Liu E, Crampin S. The mechanical properties of materials with interconnected cracks and pores. Geophys. J. Int., 1996, 124(1): 105-112.
[6]
Van der Kolk C M, Guest W S, Potters J H H M. The 3D shear experiment over the Natih field in Oman: the effect of fracture-filling fluids on shear propagation. Geophys. Prospect., 2001, 49(2): 179-197.
[7]
Chapman M. Frequency-dependent anisotropy due to meso-scale fractures in the presence of equant porosity. Geophys. Prospect., 2003, 51(5): 369-379.
[8]
Brown R J S, Korringa J. On the dependence of the elastic properties of a porous rock on the compressibility of the pore fluid. Geophysics, 1975, 40(4): 608-616.
[9]
Chapman M, Maultzsch S, Liu E R, et al. The effect of fluid saturation in an anisotropic multi-scale equant porosity model. J. Appl. Geophys., 2003, 54(3-4): 191-202.
[10]
Chapman M, Liu E R, Li X Y. The influence of fluid sensitive dispersion and attenuation on AVO analysis. Geophysical Journal International, 2006, 167(1): 89-105.
[11]
何樵登, 张中杰. 横向各向同性介质中地震波及其数值模拟. 长春: 吉林大学出版社, 1996. He Q D, Zhang Z J. Wave in Transversely Isotropic Medium and Numerical Modelling (in Chinese). Changchun: Jilin University Press, 1996.
[12]
Zhang Z J, Teng J, Badal J, et al. Construction of regional and local seismic anisotropic structures from wide-angle seismic data: crustal deformation in the southeast of China. Journal of Seismology, 2009, 13(2): 241-252.
[13]
Yang D H, Wang S Q, Zhang Z J, et al. N-times absorbing bounding conditions for compact finite-difference modeling of acoustic and elastic wave propagation in the 2D TI medium. Bull. Seismol. Soc. Am., 2003, 93(6): 2389-2401.
[14]
Yang D H, Zhang Z J. Poroelastic wave equation including the Biot/Squirt mechanism and the solid/fluid coupling anisotropy. Wave Motion, 2002, 35(3): 223-245.
[15]
Nishizawa O. Seismic velocity anisotropy in a medium containing oriented cracks-transversely isotropic case. Journal of Physics of the Earth, 1982, 30(4): 331-347.
[16]
Thomsen L. Weak elastic anisotropy. Geophysics, 1986, 51(10): 1954-1966.
[17]
Thomsen L. Elastic anisotropy due to aligned cracks in porous rock. Geophys. Prospect., 1995, 43(6): 805-829.
[18]
Tod S R. The effects on seismic waves of interconnected nearly aligned cracks. Geophysical Journal International, 2001, 146(1): 249-263.
[19]
Chapman M, Zatsepin S V, Crampin S. Derivation of a microstructural poroelastic model. Geophys. J. Int., 2002, 151(2): 427-451.
[20]
Chapman M H. Modelling the wide-band laboratory response of rock samples to fluid and pressure changes. Edinburgh: University of Edinburgh, 2001.
[21]
Champan M. Modeling the effect of multiple sets of mesoscale fractures in porous rock on frequency-dependent anisotropy. Geophysics, 2009, 74(6): D97-D103.
[22]
张中杰, 滕吉文, 贺振华. EDA介质中地震波速度、衰减与品质因子方位异性研究. 中国科学(E辑), 1999, 29(6): 569-574. Zhang Z J, Teng J W, He Z H. The detection attenuation research on seismic wave velocity ''Attenuation'' quality factor of EDA medium. Science in China (Ser. E) (in Chinese), 2009, 29(6): 569-574.
[23]
张忠杰. 多分量地震资料的各向异性处理与解释方法. 哈尔滨: 黑龙江教育出版社, 2002. Zhang Z J. Multi-component Seismic Data Anisotropic Processing and Interpretation Methods (in Chinese). Harbin: Heilongjiang Education Press, 2002.
[24]
Zhang Z J, Wang G J, Harris J M. Multi-component wavefield simulation in viscous extensively dilatancy anisotropic media. Phys., Earth Planet. Inter., 1999, 114(1-2): 25-38.
[25]
Yang D H, Liu E R, Zhang Z J, et al. Finite-difference modelling in two-dimension anisotropic media using a flux-corrected transport technique. Geophys. J. Int., 2002, 148(2): 320-328.
[26]
Zheng H S, Zhang Z J, Liu E R. Non-linear seismic wave propagation in anisotropic media using the flux-corrected transport technique. Geophysical Journal International, 2006, 165(3): 943-956.
[27]
Yang D H, Zhang Z J. Effects of the Biot and the squirt-flow coupling interaction on anisotropic elastic waves. Chinese Science Bulletin, 2000, 45(23): 2130-2138.
[28]
Lan H Q, Zhang Z J. Seismic wavefield modeling in media with fluid-filled fractures and surface topography. Applied Geophysics, 2012, 9(3): 301-312.
[29]
徐涛, 徐果明, 高尔根等. 三维复杂介质的块状建模和试射射线追踪. 地球物理学报, 2004, 47(6): 1118-1126. Xu T, Xu G M, Gao E G, et al. Block modeling and shooting ray tracing in complex 3-D media. Chinese J. Geophys. (in Chinese), 2004, 47(6): 1118-1126.
[30]
Xu T, Xu G M, Gao E G, et al. Block modeling and segmentally iterative ray tracing in complex 3D media. Geophysics, 2006, 71(3): T41-T51.
[31]
Xu T, Zhang Z J, Gao E G, et al. Segmentally iterative ray tracing in complex 2D and 3D heterogeneous block models. Bull. Seismol. Soc. Am., 2010, 100(2): 841-850.
[32]
Liu K, Zhang Z J, Hu J F, et al. Frequency band-dependence of S-wave splitting in China mainland and its implications. Science in China (Series D), 2001, 44(7): 659-665.
[33]
Maultzsch S, Chapman M, Liu E R, et al. Modelling frequency-dependent seismic anisotropy in fluid-saturated rock with aligned fractures: implication of fracture size estimation from anisotropic measurements. Geophysical Prospecting, 2003, 51(5): 381-392.
[34]
Dvorkin J, Nur A. Dynamic poroelasticity: A unified model with the squirt and the Biot mechanisms. Geophysics, 1993, 58(4): 524-533.
[35]
Tsvankin I. Anisotropic parameters and P-wave velocity for orthorhombic media. Geophysics, 1997, 62(4): 1292-1309.
