Figure 7. Close-up of Line GeoB/AWI 96-008 near Site 1087. Vertical axis is given in TWT Amplitudes are grayscaled. For comparison, the GRAPE density profile from MST measurements is shown. Depth scale is transferred to the TWT scale using the average sound velocity of 1775 m/s, derived from downhole logging. Selected reflectors can be tentatively correlated with local extremes in the core log (thick dashed lines).

Figure 7. Close-up of Line GeoB/AWI 96-008 near Site 1087. Vertical axis is given in TWT Amplitudes are grayscaled. For comparison, the GRAPE density profile from MST measurements is shown. Depth scale is transferred to the TWT scale using the average sound velocity of 1775 m/s, derived from downhole logging. Selected reflectors can be tentatively correlated with local extremes in the core log (thick dashed lines).