Figure 5. Close-up of Line GeoB/AWI 96-006 near Site 1086. Amplitudes are grayscaled. For comparison, GRAPE density data from MST measurements are shown. Many peaks may be associated with seismic reflectors (thick dashed lines). For depth determination, an average sound velocity (Vp) of 1600 m/s was used.

Figure 5. Close-up of Line GeoB/AWI 96-006 near Site 1086. Amplitudes are grayscaled. For comparison, GRAPE density data from MST measurements are shown. Many peaks may be associated with seismic reflectors (thick dashed lines). For depth determination, an average sound velocity (V_p) of 1600 m/s was used.