--> Figure 13. Relationships between seismic stratigraphic units, velocity and clay mineralogy in well 34/7-1. The Plio-Pleistocene sediments show a strong increase in velocity with depth but this is not the case in the Eocene and Oligocene smectite-rich sediments (Thyberg et al., 2000, Geological Society Special Publication, No. 167).

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Figure 13. Relationships between seismic stratigraphic units, velocity and clay mineralogy in well 34/7-1. The Plio-Pleistocene sediments show a strong increase in velocity with depth but this is not the case in the Eocene and Oligocene smectite-rich sediments (Thyberg et al., 2000, Geological Society Special Publication, No. 167).