3D Geometric Modeling of the Abu Madi Reservoirs and Its Implication on the Gas Development in Baltim Area (Offshore Nile Delta, Egypt)

Figure 16

Stratigraphic architecture of a fluvial depositional sequence influenced by base-level fluctuations for the Abu Madi incised valley channel system. Each system tract contains a fining upward succession caused by the continuous coastal aggradation and subsequent shallowing of the fluvial graded profile. List of abbreviations: lowstand system tract (LST), transgressive system tract (TST), highstand system tract (HST), maximum flooding surface (MFS), and sequence boundary (SB).