Pirmez, C., Beauboeuf, R.T., Friedmann, S.J. and Mohrig, D.C. (2000) Equilibrium Profile and Base Level in Submarine Channels: Examples from Late Pleistocene Systems and Implications for the Architecture of Deepwater Reservoirs. In: Weimer, P., Slatt, R.M., Coleman, J., Rosen, N.C., Nelson, H., Bouma, A.H., Styzen, M.J. and Lawrence, D.T., Eds., 20th Annual GCSSEPM Foundation Bob F. Perkins Research Conference 2000: Deep-Water Reservoirs of the World, Houston, 782-805.

has been cited by the following article:

• TITLE: Seismic Imaging and Reservoir Architecture of Sub-Marine Channel Systems Offshore West Nile Delta of Egypt

  AUTHORS: Essam Sharaf, Ibrahim Korrat, Hamdy Seisa, Eslam Esmaiel

  KEYWORDS: Offshore Nile Delta, Western Nile Delta, Seismic, Reservoir Architecture, Submarine Channel System

  JOURNAL NAME: Open Journal of Geology, Vol.4 No.12, December 31, 2014

  ABSTRACT: Offshore Nile Delta gas reservoirs are dominated by slope-channel systems of Plio-Pleistocene age. High-quality, three-dimensional seismic imaging has significantly helped in defining the geomorphology and architectures of these channels. Integrating seismic, logs and core data from four wells resulted in understanding of different stages of channel development and reservoir quality. The studied reservoirs that are largely controlled by episodes of transgressive-regressive events resulted in deposition of fine grained sediment and shale. Sienna channel complex consists of unconfined channel system with clearly defined development stages. The stages include amalgamated or stacked channels followed by channel abandonment phases and local flooding events. The depositional pattern continued through the Late Pliocene-Pleistocene. SimSat-P1 and SimSat-P2 reservoirs are characterized by isolated sand bodies, most probably relics of fan depositional setting. The depositional scenario that is largely controlled by successive transgression and flooding events resulted in deposition of interbedded, sheet-like, fine grained sediment and shale.