--> Relationship Between Reservoir Quality, Facies and Depositional Environment: Working Towards a Predictive Model for the Deepwater Wilcox
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Relationship Between Previous HitReservoirNext Hit Previous HitQualityNext Hit, Facies and Depositional Environment: Working Towards a Predictive Model for the Deepwater Wilcox

Abstract

Successful development of the Wilcox deepwater reservoirs is predicated on understanding the Previous HitreservoirNext Hit Previous HitqualityNext Hit distribution. Wilcox Previous HitreservoirNext Hit Previous HitqualityNext Hit is not simply a function of mechanical compaction with depth. Previous HitReservoirNext Hit intervals at similar depths below mud-line in the same well have very different Previous HitreservoirNext Hit Previous HitqualityNext Hit. In addition, the range in Previous HitreservoirNext Hit Previous HitqualityNext Hit for the most abundant Previous HitreservoirNext Hit facies, the massive sandstones or what are interpreted to be Bouma Ta turbidite divisions, was much greater than had been observed in other deepwater reservoirs. This range in Previous HitreservoirNext Hit Previous HitqualityNext Hit caused a large amount of uncertainty in predicting and modeling of permeability distribution. In response to this important business challenge, a major focus has been on significantly improving the understanding of the linkages between Previous HitreservoirNext Hit Previous HitqualityNext Hit, depositional architecture and lithofacies distribution for the Wilcox and in developing new workflows and models for improved Previous HitreservoirNext Hit description, classification and Previous HitqualityNext Hit prediction. The first step to solving this problem was a detailed classification of all the Previous HitreservoirNext Hit facies and interpretation of the Previous HitreservoirNext Hit architecture. From this analysis, it was interpreted that the best Previous HitreservoirNext Hit Previous HitqualityNext Hit was associated with channelized and proximal sheet reservoirs. It was observed that a significant amount of massive “sandstones” had large amounts of silt, which is unusual for Ta sandstones. These silty massive sandstones were more common in the interpreted sheet deposits and most common in the distal sheet setting. Preliminary analysis suggests that massive sandstones with high fine-grained content are not Ta turbidite deposits. Instead, these sandy siltstones with poorer Previous HitreservoirNext Hit Previous HitqualityNext Hit represent a transitional facies between turbidites and debrites. These transitional facies need to be treated separately from the cleaner turbidites in forward modeling of Previous HitreservoirNext Hit Previous HitqualityNext Hit. It can now be demonstrated that Previous HitreservoirNext Hit Previous HitqualityNext Hit is strongly controlled by Previous HitreservoirNext Hit architecture and in particular proximal to distal changes in depositional sand Previous HitqualityNext Hit and not solely related to mechanical compaction. This has resulted in more accurate modeling and prediction of Wilcox Previous HitreservoirNext Hit Previous HitqualityNext Hit. This fundamentally new view of the controls on Previous HitreservoirNext Hit Previous HitqualityTop has the potential to significantly impact the forward modeling of permeability distribution and impact current Wilcox developments and future exploration wells.