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Figure F38. A. Void ratio (e) versus hydrostatic vertical effective stress ('vh) for lithostratigraphic Subunit Ic at Site U1324. The reference void ratio (e0) and compression index (Cc) are derived from a fit of the type e = e0 Cc ln('vh). B. Pore pressures for Site U1322 and U1324 are derived from parameters derived in A. assuming that lithostratigraphic Subunit Ic (blue dots) at Site U1324 is hydrostatically pressured. Pore pressures recorded at the end of temperature and dual pressure probe (T2P) (red triangles) and Davis-Villinger Temperature-Pressure Probe (DVTPP) (red squares) deployments are also shown. BSF = below seafloor, RM = running mean, PP = pore pressure.
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