Hi gridder, Yes, the influence of bottom currents should also apply to the possible basin-floor fan (BFF) leads I have labelled below with associated winnowing processes to enhance reservoir quality. That said, these BFF's do not have the hummocky, wavey, undulating morphology like the turbidites within the Saturn Complex. Reworking of the BBF's may not have been as intense as the Saturn Complex as they were likely deposited in a deeper water environment when compared with the turbidites in the Saturn Complex. The turbidites of the Saturn Complex, also appear to have been deposited closer to the shelf where the bottom currents may have had a greater influence. Just my thoughts gridder; I welcome alternate views.
OldGeo
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