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Rift, Compartmentalisation and Evolution of Tilted Previous HitFaultNext Hit Blocks as Expressed by the Lower Miocene Abu Zenima and Nukhul Formations Suez Egypt


 Chris Jackson1, Rob Gawthorpe1, Mike Young1, Jim Stewart2, Dave Pivnik2, Ian Sharp1

(1) University of Manchester, Manchester, United Kingdom (2) BP (Gulf of Suez Exploration Company), Cairo, Egypt

 Although tilted Previous HitfaultNext Hit blocks are common traps within rift basins more subtle and complex structural and stratigraphic traps can be developed during Previous HitfaultNext Hit zone evolution by the growth, interaction and linkage of Previous HitfaultNext Hit segments. The early syn-rift Abu Zenima and Nukhul Formations (Lower Miocene) of the Suez Rift can be used to determine the early rift structure. Outcrop studies in the Hammam Faraun Previous HitfaultNext Hit block indicate that initial Previous HitfaultNext Hit activity was distributed across the Previous HitfaultNext Hit block on short (1-4 km long), low displacement (<1 km) segments. These initial segments either linked to form longer Previous HitfaultNext Hit zones, or became inactive during the first 6-8 Myr of rifting. Displacement progressively localised onto >25 km long border Previous HitfaultNext Hit zones that bound the present-day major tilted Previous HitfaultNext Hit block, and many of the early intra-block Previous HitfaultNext Hit zones became inactive. In the N. October and East Tanka areas in the central Gulf of Suez, the Abu Zenima and Nukhul Formations form hydrocarbon accumulations that are compartmentalized, commonly lack hydrodynamic continuity, and which have different oil/water contacts and hydrocarbon types. Reservoir distribution and compartmentalization is interpreted to reflect deposition in early Previous HitfaultNext Hit-controlled depocentres that formed prior to the development of the main faults controlling the October and East Tanka fields. Thus understanding the growth, linkage and death of Previous HitfaultTop segments and reconstruction of the early rift structure has important implications for subtle trap and reservoir distribution in rift basins.