Figure 3.Seismic cross section through Site 988 (top). Interpretations shown in line drawing (middle) and migrated section (bottom). The Eocene age of the postrift sediments is inferred through correlation with the EG63 transect (Larsen, Saunders, Clift et al., 1994). Seismic velocities used in the depth conversion and migration are in km/s.

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