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In Omatsola and Adegoke (1981), a three-stage development has been proposed (Fig. 4a, b, c). A model for developing the basin (Fig. 4) indicating the stages of the basin subsidence and sediment deposition was proposed by Omatsola and Adegoke (1981). Doust and Omatsola (1990) describe three depobelt provinces based on structure. The northern delta province, which overlies relatively shallow basement, has the oldest growth faults that are generally rotational, evenly spaced, and increase their steepness seaward. (2013) studied the petroleum geology of the Fula sub-basin (northeastern part of the Muglad Basin). Fairhead et al. (2013) investigated the role that plate tectonics, inferred stress changes and stratigraphic unconformities played in the evolution of the WCARS and the Atlantic continental margins. Dong et al. There are two types of properties that will be used in reservoircharacterization, they are petrophysical (porosity, shale volume, watersaturation,permeability) and seismic - rock physics (elasticity, wave velocity). Someapproaches are needed tocharacterize reservoir by using well logs data to calculate. A total of twenty-four (24) reservoir sand bodies with variable net thicknesses varying from 25-150m in places had been inferred. The average net thickness (h), porosity, effective porosity, clay volume and water saturation of 135m (approximately 473ft), 0.26, 0.22, 0.16 and 0.00252, respectively were estimated. The 3D seismic amplitude data covers an area of about 421 sq. km in the onshore area of the Niger Delta. The bin spacing of the data is 25 by 25 m. The data are available in milliseconds two-way travel time (ms TWTT) with a maximum value of 3000 ms. It has Inline range of 11228 12110 and Crossline range of 2673 3434 (Figure 1.3). The un- discovered resources of the Tertiary Niger Delta (Akata-Agbada) Petro- leum System is estimated at 40.5 billion barrels of oil and 133 trillion cubic feet of gas (Michael and Ronald, 2006). Ejedaweet al. (1984), suggestedthat theAgbadashale sourcesthe oil while the Akata shale sources the gas. Department of Geology, University of Port Harcourt, Nigeria et al. (2013). As an important petroleum provider and greenhouse emitter in Africa, hydrocarbon exploration and production in Nigeria since 1957 has led to depletion and abandonment Stauble (1967) and Doust and Omatsola (1990). The lithostratigraphic subdivision of the The best studied of these is the petroliferous Agbada Formation with its varied lithofacies associations that range from reservoir sands through heteroliths to mudrock seal facies. The Niger Delta is a hydrocarbon province with ultimate recovery presently estimated at nearly 40 billion barrels of oil. Mascle, 1976; Omatsola and Adegoke, 1981; Mascle et al., 1988; Tucker, 1992; Chierici, 1996; Eaglesand Konig, 2008; Moulin et al., 2010). Seismic and bore h*** data show that sedimentary fill within the Basin is more than 3500 m thick. The stratigraphy of the OBB has been discussed by various workers (Hessouh et al., 1994; Kaki et al., 2001 tains only one petroleum system called the Ak