72nd EAGE Conference and Exhibition Incorporating SPE EUROPEC 2010 2010
DOI: 10.3997/2214-4609.201400685
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Velocity-independent "tau"-p Moveout in a Layered VTI Medium

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Cited by 6 publications
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“…The non-hyperbolic form of this approximation allows computing the additional * E-mail: alexey.stovas@ntnu.no parameter related to effective heterogeneity or anisotropy. The case of 3-D elliptical anisotropy was considered by Burnett and Fomel (2009) and Casasanta (2011). The case of vertical transverse isotropy (VTI) was considered by Casasanta and Fomel (2011).…”
Section: Introductionmentioning
confidence: 99%
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“…The non-hyperbolic form of this approximation allows computing the additional * E-mail: alexey.stovas@ntnu.no parameter related to effective heterogeneity or anisotropy. The case of 3-D elliptical anisotropy was considered by Burnett and Fomel (2009) and Casasanta (2011). The case of vertical transverse isotropy (VTI) was considered by Casasanta and Fomel (2011).…”
Section: Introductionmentioning
confidence: 99%
“…The case of 3-D elliptical anisotropy was considered by Burnett and Fomel (2009) and Casasanta (2011). The case of vertical transverse isotropy (VTI) was considered by Casasanta and Fomel (2011).…”
Section: Introductionmentioning
confidence: 99%
“…Khoshnavaz et al (2016a) proposed to use predictive painting (Fomel 2010) of local slopes to estimate the kinematic attributes, which substitutes the need for curvatures by using the result of predictive painting. The local slopes are also applied to other steps of seismic data processing and imaging (Cooke et al 2009;Bóna 2011;Khoshnavaz et al 2016b;Khoshnavaz 2017;Decker et al 2017;Casasanta and Fomel 2011). The local slopes can be obtained by so-called plane-wave destruction (PWD) (Claerbout 1992;Fomel 2002;Fomel and Stovas 2010).…”
Section: Introductionmentioning
confidence: 99%
“…Local data slopes were used for tomographic velocity model building by Sword (1987) and later extended in the method of stereo-tomography by Billette and Lambaré (1998), Billette et al (2003) and Lambaré et al (2004). Slope estimation in data were used for depth imaging (Baina et al 2003), moveout correction (Casasanta and Fomel 2011), time imaging (Fomel 2007) and fast beam migration (Sherwood et al 2009;Duchkov, Andersson and Ojala 2012). Slopes in a seismic stack were used for parsimonious migration in Hua and McMechan (2003).…”
Section: Introductionmentioning
confidence: 99%
“…Slope estimation in data were used for depth imaging (Baina et al . ), moveout correction (Casasanta and Fomel ), time imaging (Fomel ) and fast beam migration (Sherwood et al . ; Duchkov, Andersson and Ojala ).…”
Section: Introductionmentioning
confidence: 99%