SEG Technical Program Expanded Abstracts 1993 1993
DOI: 10.1190/1.1822290
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Multiple weights in diffraction stack migration

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Cited by 10 publications
(19 citation statements)
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“…(18) is a high-frequency approximation of the back-propagated wavefield that does not require the wave-mode expansion (2) or the integration over the reflector R. Even though this equation and its time-domain counterpart (19) are still applicable to elastic wave propagation in general anisotropic media, they have the very appealing form of a multipleweighted reverse-time (back propagated) diffraction stack of the transformed data given by Eq. (20) (Tygel et al, 1993). The factor c (r) (Eq.…”
Section: Stationary-phase Conditionsmentioning
confidence: 99%
“…(18) is a high-frequency approximation of the back-propagated wavefield that does not require the wave-mode expansion (2) or the integration over the reflector R. Even though this equation and its time-domain counterpart (19) are still applicable to elastic wave propagation in general anisotropic media, they have the very appealing form of a multipleweighted reverse-time (back propagated) diffraction stack of the transformed data given by Eq. (20) (Tygel et al, 1993). The factor c (r) (Eq.…”
Section: Stationary-phase Conditionsmentioning
confidence: 99%
“…Thus, when P is coincident with R, the depth-migrated image given in equation (B-1) in Tygel et al (1993) is zero, independent of the weight function used. Because of this fact, at R the ratio between any two depth-migrated images has the form of 0/0.…”
Section: True-amplitude Migration Without Distortionmentioning
confidence: 95%
“…If the seismic signal is a causal wavelet, the vector diffraction stack published in Tygel et al (1993) breaks down at an actual reflection point. Consequently, only the seismic parameters underneath the target reflector can be estimated properly.…”
Section: True-amplitude Migration Without Distortionmentioning
confidence: 99%
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