Author(s)

Essam Sharaf¹, Ibrahim Korrat¹, Hamdy Seisa¹, Eslam Esmaiel²

¹Geology Department, Faculty of Science, Mansoura University, Mansoura, Egypt.
²Department of Production Management, PETRONAS (PICL) Egypt, Helwan, Egypt.

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.

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

Sharaf, E. , Korrat, I. , Seisa, H. and Esmaiel, E. (2014) Seismic Imaging and Reservoir Architecture of Sub-Marine Channel Systems Offshore West Nile Delta of Egypt. Open Journal of Geology, 4, 718-735. doi: 10.4236/ojg.2014.412052.