SEG Technical Program Expanded Abstracts 2015 2015
DOI: 10.1190/segam2015-5906814.1
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A method for converted wave receiver statics correction in the CRG domain

Abstract: A method for receiver statics correction of converted waves (PS-waves) is proposed here. It is based on the observation that the static time delay on PS-wave events between two adjacent receivers, after the source statics correction has been applied, should correspond mostly to the differential receiver statics. The surface consistent statics model provides the theoretical framework. Adjacent Common Receiver Gathers (CRG) are crosscorrelated to obtain their time delay, namely their differential receiver static… Show more

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Cited by 4 publications
(2 citation statements)
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“…The first one requires a known shear velocity model, usually obtained by direct measurements (borehole data, refraction, Rayleigh wave inversion). The second one assumes a surface consistent model, as in the statics correction methods available for acoustic wave processing (Guevara et al, 2015). However, the surface consistent assumption is not always valid, and, in the case of PS-CW, it causes error during processing.…”
Section: Introductionmentioning
confidence: 99%
“…The first one requires a known shear velocity model, usually obtained by direct measurements (borehole data, refraction, Rayleigh wave inversion). The second one assumes a surface consistent model, as in the statics correction methods available for acoustic wave processing (Guevara et al, 2015). However, the surface consistent assumption is not always valid, and, in the case of PS-CW, it causes error during processing.…”
Section: Introductionmentioning
confidence: 99%
“…Arguably more justifiable are approaches which analyse horizon-timing differences on common-receiver-gathers (CRGs) (Cary and Eaton, 1993), or methods using PPS and SSS refractions (Houston et al, 1989;Liu and Wei, 2008). More recent areas of study include a technique based on correlation of adjacent CRGs (Guevara et al, 2015); ray-path interferometry via the radial trace or Tau-p domains (e.g. Henley, 2014;Cova et al, 2015); and inversion of surface-wave dispersion data (e.g.…”
mentioning
confidence: 99%