Poroelastic finite difference modeling of seismic attenuation and dispersion due to mesoscopic-scale heterogeneity

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Quasi-static finite element modeling of seismic attenuation and dispersion due to wave-induced fluid flow in poroelastic media (2011, methodology): “[6] In this study, we modified and elaborated the method suggested by Masson and Pride [2007] .”
An unsplit convolutional perfectly matched layer improved at grazing incidence for seismic wave propagation in poroelastic media (2008, methodology): “…simulation of wave propagation in genral heterogeneous poroelastic media, the finite-difference method s probably the most widely used technique e.g., Zhu and Mc- echan, 1991; Dai et al., 1995; Jianfeng, 1999; Pride et al., 2004; asson et al., 2006; Sheen et al., 2006; Masson and Pride, 2007 .”