2014
DOI: 10.3997/2214-4609.20140648
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S-ray Approximation Tomography for PP and PS Horizon Co-Depthing

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Cited by 5 publications
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“…Defocusing is caused by a residual sloping up (Figure 7b, left) and down (Figure 7b, right) of energy in the CIGs, resulting in amplitude cancellation after stack. These slopes, supplied to a joint PP-PS inversion with codepthing constraints (D'Afonseca et al, 2014), can produce an anisotropy update that will result in better PP and PS images. Moreover, because of the asymmetric nature of PS propagation, stacks from opposite azimuthal directions can show image misalignments that can be used as additional constraints in a tomographic inversion.…”
Section: Ps Model Buildingmentioning
confidence: 99%
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“…Defocusing is caused by a residual sloping up (Figure 7b, left) and down (Figure 7b, right) of energy in the CIGs, resulting in amplitude cancellation after stack. These slopes, supplied to a joint PP-PS inversion with codepthing constraints (D'Afonseca et al, 2014), can produce an anisotropy update that will result in better PP and PS images. Moreover, because of the asymmetric nature of PS propagation, stacks from opposite azimuthal directions can show image misalignments that can be used as additional constraints in a tomographic inversion.…”
Section: Ps Model Buildingmentioning
confidence: 99%
“…V S then is obtained by imposing a 1D vertical codepthing constraint and inversion. In complex geology, a ray-based solution (D'Afonseca et al, 2014) can obtain a more plausible V S field by imposing codepthing in a 3D sense. In addition, a 3D displacement field that describes the relative shifts between events on the PP and PS CIGs can be incorporated as an additional constraint into a tomographic inversion (Mathewson et al, 2013).…”
Section: Ps Model Buildingmentioning
confidence: 99%