27-28 October 2017 | Muscat, Oman
Field trip seats are very limited – please book your place well in advance to avoid disappointment.
Field development requires certain decisions to be made depending on field life and each decision will require a specific type of model. The field trip will focus on aspects of sediment body geomentry, facies and linked reservoir properties as well as field scale barriers and baffles.
The Upper Gharif Formation is composed of fluvial sandstones with an overlying incised valley fill estuarine sequence leading to transgression of Khuff Carbonates. Stacking of channels, net to gross and potential barriers and baffles can be observed in these outcrops as well as facies variations.
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