Figure F54. Synthetic seismogram plotted on line MAR13 with two-way traveltime-to-depth velocity data, P-wave velocity and gamma ray attenuation bulk densities, extracted sonic wavelet, synthetic seismogram, the megasequence boundaries, and lithologic boundaries. The traveltime-vs.-depth plot was used to correlate seismic reflection events to their location with depth in the sedimentary section.

Figure F54. Synthetic seismogram plotted on line MAR13 with two-way traveltime-to-depth velocity data, P-wave velocity and gamma ray attenuation bulk densities, extracted sonic wavelet, synthetic seismogram, the megasequence boundaries, and lithologic boundaries. The traveltime-vs.-depth plot was used to correlate seismic reflection events to their location with depth in the sedimentary section.