Anisotropy signature in P-wave extended images for VTI media
نویسندگان
چکیده
Extended images obtained from reverse-time migration (RTM) contain information about the accuracy of the velocity field and subsurface illumination at different incidence angles. Here, we evaluate the influence of errors in the anisotropy parameters on the residual moveout (RMO) in P-wave extended images obtained with RTM for VTI (transversely isotropic with a vertical symmetry axis) media. Assuming the actual spatial distribution of the zero-dip normal-moveout velocity, we analyze extended images computed with distorted fields of the parameters η and δ. Differential semblance optimization (DSO) and stack-power criteria are employed to study the sensitivity of focusing to the anisotropy parameters. The results show that the signature of η is dip-dependent, whereas errors in δ cause defocusing in extended images only if that parameter varies laterally. We also obtain and analyze the gradients of the DSO objective function with respect to the anisotropy parameters. The results of this work provide the foundation for anisotropic wavefield tomography operating with extended images. Summary Introduction The extended imaging condition retains information about the wavefield directionality and angle-dependent reflector illumination by preserving the spatial and/or temporal correlation lags in the output. For example, one can obtain space-lag (Rickett and Sava, 2002) or time-lag (Sava and Fomel, 2006) extended common-image gathers (CIG), which are computed at fixed horizontal coordinates.
منابع مشابه
Elastic wave-mode separation for VTI media
Elastic wave propagation in anisotropic media is well represented by elastic wave equations. Modeling based on elastic wave equations characterizes both kinematics and dynamics correctly. However, because P and S modes are both propagated using elastic wave equations, there is a need to separate P and S modes to obtain clean elastic images. The separation of wave modes to P and S from isotropic...
متن کاملRange of the P - wave anisotropy parameter for nely layered VTI
Since the work of Postma (1955) and Backus (1962), much is known about elastic constants in vertical transversely isotropic (VTI) media when the anisotropy is due to ne layering of isotropic elastic materials. I review earlier work and then show that the P-wave anisotropy parameter c 11 =c 33 lies in the range 1 4 c 11 =c 33 h + 2i h1=(+ 2)i, when the layers are themselves composed of isotropic...
متن کاملTime-domain anisotropic processing in arbitrarily inhomogeneous media
In transversely isotropic media with a vertical axis of symmetry (VTI media), we can represent the image in vertical time, as opposed to depth, thus eliminating the inherent ambiguity of resolving the vertical P-wave velocity from surface seismic data. In this new (x − τ )-domain, the raytracing and eikonal equations are completely independent of the vertical P-wave velocity, on the condition t...
متن کاملAnalytic study of the effective parameters for determination of the NMO velocity function in transversely isotropic media
In their studies of transversely isotropic media with a vertical symmetry axis (VTI media), Alkhalifah and Tsvankin observed that, to a high numerical accuracy, the normal moveout (NMO) velocity for dipping reflectors as a function of ray parameter p depends mainly on just two parameters, each of which can be determined from surface P-wave observations. They substantiated this result by using t...
متن کاملThe space±time domain: theory and modelling for anisotropic media
In transversely isotropic media with a vertical axis of symmetry (VTI media), we represent the image in vertical time, as opposed to depth, thus eliminating the inherent ambiguity of resolving the vertical P-wave velocity from surface seismic data. In this new (x±t)-domain, the ray tracing and eikonal equations are completely independent of the vertical P-wave velocity, with the condition that ...
متن کامل