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Reasons from grain-scale hydraulics, facies associations, and base-level accommodation through measured sections, Folk & Ward granulometry, Bouma divisions, ichnofacies, and core-log-seismic ties while treating diagenetic overprint, bioturbation-destroyed laminae, fining-upward and shale-equals-deep-water defaults, and single-outcrop overextrapolation as first-class failure modes.