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Figure F10. Core photograph of interbedded clayey silt (55–51 and 45–40 cm) and very fine grained sand with sharp bases that have locally been flushed during core splitting (50–45 cm) and low-angle subparallel lamination (interval 313-M0028A-92R-2, 35–55 cm). The environment of deposition is interpreted as a storm-influenced shoreface–offshore transition zone.

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