Figure 12. Comparison of a seismic profile across Site 1082 with the position of lithified layers, as seen in the sound velocity profile of downhole logging. Selected reflectors can be correlated with local extremes in the velocity log (dashed lines) and may indicate the presence of lithified intervals or dolomite clays.

Figure 12. Comparison of a seismic profile across Site 1082 with the position of lithified layers, as seen in the sound velocity profile of downhole logging. Selected reflectors can be correlated with local extremes in the velocity log (dashed lines) and may indicate the presence of lithified intervals or dolomite clays.