Proceedings of Middle East Oil Show 1993
DOI: 10.2523/25580-ms
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Geologic Modelling for Reservoir Simulation: Hanifa Reservoir, Berri Field, Saudi Arabia

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Cited by 8 publications
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“…We identified eight distinct depositional facies in the study area (Figure 3) based on their sedimentary structure, depositional texture (Dunham and Ham 1962;Embry and Klovan 1971), skeletal and nonskeletal components (Hughes, Varol, and Al-Khalid 2008), and gamma-ray response. These depositional facies are modifications from the Hanifa depositional facies identified by Al-Mojel, Razin, and Dera (2020) and the subsurface Hanifa reservoir facies (including documented porosity and permeability) by Kompanik et al (1993) and Al-Khalifah and Makkawi (2002).…”
Section: Depositional Facies and Stratigraphymentioning
confidence: 66%
“…We identified eight distinct depositional facies in the study area (Figure 3) based on their sedimentary structure, depositional texture (Dunham and Ham 1962;Embry and Klovan 1971), skeletal and nonskeletal components (Hughes, Varol, and Al-Khalid 2008), and gamma-ray response. These depositional facies are modifications from the Hanifa depositional facies identified by Al-Mojel, Razin, and Dera (2020) and the subsurface Hanifa reservoir facies (including documented porosity and permeability) by Kompanik et al (1993) and Al-Khalifah and Makkawi (2002).…”
Section: Depositional Facies and Stratigraphymentioning
confidence: 66%
“…At Berri Field, the formation contains an excellent reservoir facies which consists of skeletal-bioclastic grainstone. Permeabilities are of value up to 10 D and the formation contains large petroleum reserves (Kompanik et al 1993).…”
Section: Jurassicmentioning
confidence: 99%
“…Table 2 and Fig Among these five depositional facies in the Hanifa formation, FC1 depositional facies is the only nonreservoir rock with wackestone/mudstone, the remaining facies (FC2-FC5a) are reservoir rocks with fairly distinct porosity and permeability populations. Among them, FC4 depositional facies is characterized by stromatoporoid and coral fossils, and the others (FC2, FC3 and FC5a) are grain-dominated rocks (Kompanik et al, 1993).…”
Section: Automatic Depositional Facies Predictionmentioning
confidence: 99%