--> Reservoir Quality Variations Within a Sinuous Deepwater Channel System in the Niger Delta Basin, Offshore Western Africa
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Previous HitReservoirNext Hit Quality Variations Within a Sinuous Deepwater Channel Previous HitSystemNext Hit in the Niger Delta Basin, Offshore Western Africa

Abstract

Submarine fan channel reservoirs exhibit strong heterogeneity not only on channel architecture but also on the qualities of reservoirs, which can exert direct control over the fluid flow and remaining oil distribution during oilfield development. However, the distribution of the variations in the Previous HitreservoirNext Hit quality within submarine fan channel systems is poorly understood. This paper, which takes the submarine fan channel reservoirs of the X oilfield in the Niger Delta Basin as an example, aims to study the variations in Previous HitreservoirNext Hit qualities and the controlling mechanisms within a sinuous deep-water channel Previous HitsystemNext Hit. The studies are based on the integration of core analysis, well-logging interpretation, seismic inversion and interpretation constrained by channel architecture. The results show that variations in the Previous HitreservoirNext Hit quality within a sinuous deep-water channel Previous HitsystemNext Hit are primarily controlled by rock texture, lithofacies (association) and channel architecture under the circumstance of weak diagenesis. (1) The grain sorting and clay content essentially control the Previous Hitreservoir'sNext Hit porosity and permeability, respectively, while the relationship between grain size and the Previous Hitreservoir'sNext Hit properties is complicated because of the strong heterogeneity in the rock textures for different lithofacies. Cross-laminated fine sandstones have the highest porosity because of their good sorting, while massive medium to coarse sandstones have the highest permeability because of their low clay content. (2) Channel fillings are divided into four types (Type I~ Type IV), which bear different Previous HitreservoirNext Hit qualities according to the lithofacies associations. Within a complete channel Previous HitsystemNext Hit, the channel fill types evolve progressively upward as the dominant gravity flow types evolve, which leads to the worst physical properties for the Previous HitreservoirNext Hit in the early and late stages, the highest permeability in the middle stage, and the highest porosity in the middle-late stage of the target channel Previous HitsystemTop. (3) The relatively high porosity-permeability zones in the plane of a channel belt exhibit two patterns: multiple lenticular strips and single lenticular strips, which are controlled by the channel's architecture.