Figure 10. Close-up of Line GeoB/AWI 96-015 near Site 1082. Vertical axis is given in TWT. Amplitudes are grayscaled. For comparison, the sound velocity profile from downhole logging is shown. Logging depth is transferred to TWT using the logging results. Selected reflectors can be correlated with local extremes in the velocity log (thick dashed lines), but density-controlled lithologic changes are not reflected in the logging data.

Figure 10. Close-up of Line GeoB/AWI 96-015 near Site 1082. Vertical axis is given in TWT. Amplitudes are grayscaled. For comparison, the sound velocity profile from downhole logging is shown. Logging depth is transferred to TWT using the logging results. Selected reflectors can be correlated with local extremes in the velocity log (thick dashed lines), but density-controlled lithologic changes are not reflected in the logging data.