2
Physical Properties of Marine Sediments
48
Fig. 2.13 Full waveform ultrasonic core logging, from lithology controlled single traces to the gray shaded pixel graphic of transmission seismograms, and P-wave
velocity and attenuation logs derived from the transmission data. The single traces on the left-hand side reflect true amplitudes while the wiggle traces of the core
segment and the pixel graphic are normalized to maximum values. Data from Breitzke et al. (1996).
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