2019
DOI: 10.1111/1365-2478.12822
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Source wavelet correction for practical Marchenko imaging: A sub‐salt field‐data example from the Gulf of Mexico

Abstract: Imaging a target zone below a salt body can be challenging because large velocity contrasts in the overburden between the salt and surrounding sediments generate internal multiples, which interfere with primary reflections from the target level in the imaging process. This can lead to an erroneous interpretation of reflections in the sub‐salt area if multiples are misinterpreted as primaries. The Marchenko redatuming method may enable imaging of the sub‐salt target area where the effect of the multiply‐scatter… Show more

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Cited by 3 publications
(3 citation statements)
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References 52 publications
(146 reference statements)
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“…Finally, other challenges specific to the solution of the Marchenko equations such as knowledge and deconvolution of the source wavelet and removal of free-surface multiples are inherently similar to both 2D and 3D applications. Several solutions have been proposed in previous field data applications, both in terms of data pre-processing (Ravasi, 2019;Jia et al, 2018a;Staring et al, 2018;Mildner et al, 2019;Staring and Wapenaar, 2020), as well as modification of the underlying redatuming scheme (Ravasi, 2017;Slob and Wapenaar, 2017;Vargas et al, 2021) which could be directly applied in a 3D context. Perhaps more poorly understood right now is the impact of attenuation on the solution of the Marchenko equations (Slob, 2016): whilst simple amplitude-based data compensations have proven su cient so far in 2D field data application, the e↵ect of attenuation on the solution of the 3D Marchenko equations requires additional studies and will be subject of future research.…”
Section: Geophysical Aspects Of Mdc-based Inversion Workflowsmentioning
confidence: 99%
“…Finally, other challenges specific to the solution of the Marchenko equations such as knowledge and deconvolution of the source wavelet and removal of free-surface multiples are inherently similar to both 2D and 3D applications. Several solutions have been proposed in previous field data applications, both in terms of data pre-processing (Ravasi, 2019;Jia et al, 2018a;Staring et al, 2018;Mildner et al, 2019;Staring and Wapenaar, 2020), as well as modification of the underlying redatuming scheme (Ravasi, 2017;Slob and Wapenaar, 2017;Vargas et al, 2021) which could be directly applied in a 3D context. Perhaps more poorly understood right now is the impact of attenuation on the solution of the Marchenko equations (Slob, 2016): whilst simple amplitude-based data compensations have proven su cient so far in 2D field data application, the e↵ect of attenuation on the solution of the 3D Marchenko equations requires additional studies and will be subject of future research.…”
Section: Geophysical Aspects Of Mdc-based Inversion Workflowsmentioning
confidence: 99%
“…The idea of reproducing full wavefield responses from virtual sources at depth using focusing operators as presented in the previous section requires several key preprocessing steps that may introduce inaccuracies or even hinder the implementation of Marchenko redatuming in real data sets (Ravasi et al, 2016;da Costa Filho et al, 2017;Jia et al, 2018;Mildner et al, 2019a). The original approach demands knowledge of the acquisition wavelet and dense spatial distribution of sources and receivers.…”
Section: Band-limited Wavefield Extrapolationmentioning
confidence: 99%
“…Attempts of marine field data applications still show seismic-like results, however, without offering any proof of correct multiple elimination (e.g. Ravasi et al, 2016;Jia et al, 2018;Mildner et al, 2019;Staring et al, 2020). Assessing the results can be challenging without a reference, especially, when multiples generate complex interference patterns dominated by specific frequencies.…”
Section: Data-driven Multiple Eliminationmentioning
confidence: 99%