2015
DOI: 10.1190/geo2014-0014.1
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Five ways to avoid storing source wavefield snapshots in 2D elastic prestack reverse time migration

Abstract: Five alternative algorithms were evaluated to circumvent the excessive storage requirement imposed by saving source wavefield snapshots used for the crosscorrelation image condition in 2D prestack elastic reverse time migration. We compared the algorithms on the basis of their ability, either to accurately reconstruct (not save) the source wavefield or to use an alternate image condition so that neither saving nor reconstruction of full wavefields was involved. The comparisons were facilitated by using the sam… Show more

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Cited by 104 publications
(43 citation statements)
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“…It is intrinsically handled in conventional FWI by utilizing the full source wavefield with all its complexity. However, an intermediate solution of storing more than one maximum of the source wavefield also can ameliorate the excitation method in the presence of multipath (Jin et al, 2015;Nguyen and McMechan, 2015).…”
Section: Multipathing: a Shortcoming Of Excitation Approximationmentioning
confidence: 99%
“…It is intrinsically handled in conventional FWI by utilizing the full source wavefield with all its complexity. However, an intermediate solution of storing more than one maximum of the source wavefield also can ameliorate the excitation method in the presence of multipath (Jin et al, 2015;Nguyen and McMechan, 2015).…”
Section: Multipathing: a Shortcoming Of Excitation Approximationmentioning
confidence: 99%
“…Therefore, it is hard to segregate the excitation time of P-wave in elastic media. As suggested by Nguyen and McMechan (2015) in the context of reverse time migration, we compute excitation time of the divergence of wavefields ( S ∇ ), which includes only Pwave motions. Next, we store the original displacement wavefield at this excitation time.…”
Section: P-wave Exa In Elastic Fwimentioning
confidence: 99%
“…To perform the inversion on such a large 3D area, we solve the first-order acoustic wave equations using the staggered grid finite-difference method with domain decomposition (Bohlen, 2002). Among the many ways to avoid storing the huge forward (source) wavefields (Nguyen and McMechan, 2015) in 3D FWI, we choose the time- frequency hybrid domain approach (Sirgue et al, 2008), in which the forward and backward wavefields are transformed to the frequency domain on the fly so that we can calculate the gradient direction in the frequency domain within the desired frequency band. To scale the gradient direction, the diagonal of pseudo-Hessian matrix is used (Shin et al, 2001).…”
Section: Real Data Application: North Sea Obc Datamentioning
confidence: 99%