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Geomechanical tests of three well-characterized, clay-rich, macroscopically undeformed samples document the loading history and permeability of two late Miocene samples above the décollement zone and a late Oligocene sample below the ment zone of the Barbados accretionary prism. These samples are similar in all aspects studied. About two-thirds sample is clay, of which most is mixed-layer illite/smectite. Permeabilities are low, ranging from 5 × 10–18 to 1 × 10–19/m2. All samples are underconsolidated and may have been overpressured since shortly after deposition, especially the late Miocene sample near the deformation front (Site 949). Alternatively, the apparent low consolidation state may arise from disruption of grain contacts by early deformation in the accretionary prism, thereby erasing any earlier stress history.

Hydrostatic consolidation tests of undeformed, clay-rich samples from the Barbados accretionary prism, Leg 156