Figure F6. Segment of the 3.5 kHz data acquired in the first slope basin near Site U1325 showing a transparent layer at the seafloor (~5–7 m thick) representing the most recent Holocene sedimentation. A small blank zone is also identified in the center of the basin on top of a buried ridge of accreted sediments (see Fig. F7A). V.E. = vertical exaggeration.
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