SEG Technical Program Expanded Abstracts 2011 2011
DOI: 10.1190/1.3627868
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Improving atlantis TTI model building: OBN+NATS, prism waves & 3D RTM angle gathers

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Cited by 14 publications
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“…Like many subsalt fields in the GoM, seismic imaging at Atlantis is very challenging due to complex salt structures in the overburden (Figure 1). Recently, great efforts were made to obtain a better tilted transverse isotropic (TTI) velocity model for the Atlantis field using multi-wide azimuth and ocean-bottom node (OBN) data (Roberts et al, 2011;Shen et al, 2017). Yet 3D vertical seismic profile (VSP) surveys may offer even better opportunities to obtain high-quality images near the wellbore compared to surface steamer and OBN data due to the fact that the wave propagation is less distorted by salt since the receivers are generally placed below the salt.…”
Section: Introductionmentioning
confidence: 99%
“…Like many subsalt fields in the GoM, seismic imaging at Atlantis is very challenging due to complex salt structures in the overburden (Figure 1). Recently, great efforts were made to obtain a better tilted transverse isotropic (TTI) velocity model for the Atlantis field using multi-wide azimuth and ocean-bottom node (OBN) data (Roberts et al, 2011;Shen et al, 2017). Yet 3D vertical seismic profile (VSP) surveys may offer even better opportunities to obtain high-quality images near the wellbore compared to surface steamer and OBN data due to the fact that the wave propagation is less distorted by salt since the receivers are generally placed below the salt.…”
Section: Introductionmentioning
confidence: 99%
“…Another application of RTM 3D dip gathers of point diffractors is in subsalt illumination compensation and noise attenuation. Although wide azimuth and full azimuth acquisitions (Michell et al, 2006;Roberts et al, 2011;Tim, 2011), together with advances in RTM (Zhang et al, 2007;Zhang and Zhang, 2009), have brought significant advancements in subsalt imaging in the GOM, we continue to see poor subsalt images of weak illumination in the presence of complex salt structures (Gherasim et al, 2010;Shen et al, 2011;. Starting with a reflectivity model M and a velocity model, a field acquisition acquiring seismic data D can be simulated with a forward modeling operator F in the form of…”
Section: Introductionmentioning
confidence: 99%