Figure F14. Distribution of bedding dip angles and deformation structures with depth. Shaded band = fractured/brecciated zone associated with the splay fault. Two inversions of biostratigraphic ages occur near the upper and lower boundaries of the fractured/brecciated zone. Note the relatively small number of structural measurement in the prism sediments at 100–256 m core depth below seafloor (CSF) because of drilling-induced brecciation and poor core recovery.
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