Figure F5. Example of the seismic to core correlation (Site 1259), as conducted with a synthetic seismogram (from Erbacher, Mosher, Malone, et al., 2004). The synthetic seismogram was generated using merged data from drill site check shot, logging, and core measured velocity and density data, convolved with an idealized Ormsby wavelet. No attempt was made at simulating multiple path reflections, nor amplitude preservation. Using sediment acoustic velocities derived from this correlation, the seismic data were migrated to the depth domain. Each site was correlated in a similar manner.

Figure F5. Example of the seismic to core correlation (Site 1259), as conducted with a synthetic seismogram (from Erbacher, Mosher, Malone, et al., 2004). The synthetic seismogram was generated using merged data from drill site check shot, logging, and core measured velocity and density data, convolved with an idealized Ormsby wavelet. No attempt was made at simulating multiple path reflections, nor amplitude preservation. Using sediment acoustic velocities derived from this correlation, the seismic data were migrated to the depth domain. Each site was correlated in a similar manner.