2001
DOI: 10.1046/j.1365-2397.2001.00136.x
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Velocity as an attribute: continuous velocity estimation from 3D preSDM CRP gathers

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Cited by 7 publications
(2 citation statements)
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“…Taking the CRP gathers from the two surveys, after final migration with a common velocity model, we ‘backed‐out’ the migration velocity field, by applying inverse NMO to the otherwise flat CRP gathers. A dense velocity analysis technique ( Adler 1999; Jones & Baud 1999) was then used to yield independent velocity estimates on an 18.75 m × 12.5 m grid. The percentage differences in velocity for the base chalk event are shown in Fig.…”
Section: Azimuthal Velocity Differences Between the Two Surveysmentioning
confidence: 99%
“…Taking the CRP gathers from the two surveys, after final migration with a common velocity model, we ‘backed‐out’ the migration velocity field, by applying inverse NMO to the otherwise flat CRP gathers. A dense velocity analysis technique ( Adler 1999; Jones & Baud 1999) was then used to yield independent velocity estimates on an 18.75 m × 12.5 m grid. The percentage differences in velocity for the base chalk event are shown in Fig.…”
Section: Azimuthal Velocity Differences Between the Two Surveysmentioning
confidence: 99%
“…Previously, one of us (Jones & Baud 2001) demonstrated the potential of using a dense velocity estimate as a high-resolution tool for visualizing subtle changes not clearly discernable in the seismic amplitude response. (The success of such techniques depends to a large part on the data being correctly pre-stack migrated, so that all the diffraction energy is correctly collapsed.…”
Section: Introductionmentioning
confidence: 99%