Reverse time migration for vertical transversely isotropic media
Abstract
One of the main assumptions for solving wave equation either numerically or analytically is to compensate the anisotropic properties which are usually observed in the earth materials. Consequently, most conventional prestack depth migration techniques based on wave equation solution are not sufficient for these anisotropic media.
Asymptotic analysis of wave propagation in vertical transversely isotropic (VTI) media yields a dispersion relation of couple P- and SV wave modes that can be converted to a fourth order scalar partial differential equation (PDE). By setting the shear wave velocity equal 0 and defining the auxiliary function, the fourth order PDE acoustic wave equation for VTI media can be reduced to a system of coupled second order PDEs and then can be solved numerically by finite difference method (FDM). The result of this P wavefi eld simulation is kinematically similar to the one of elastic VTI wavefield simulation.
Since the FDM approach can simulate the wavefield propagation in the VTI media, and reverse time migration (RTM) images the reflectors by using time extrapolation to synthesise source and receiver wavefield in the subsurface by FDM, the RTM technique is then promptly suggested to image the subsurface. The accuracy of subsurface imaging of the proposed algorithm has been verified by VTI Marmousi synthetic example.
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