33. Sedimentary Sequences Influenced by Submarine Fan Deposition: Argo Abyssal Plain, Northwestern AUSTRALIA1

Transition probabilities from both core descriptions and wireline-log data from the Miocene section of Ocean Drilling Program Leg 123 Site 765 are examined. The data cover 270 m of section dominated by carbonate turbidites with varying silica content. Although the significant transitions do not echo the "classic" Bouma sequence, statistically significant cycles and pair-oscillation appear to be common when substitution