“…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.…”