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• W2181433680 abstract "The Sarvak Formation (Albian-Turonian) was measured 822 m in type section and mainly consists of carbonate rocks. This Formation forms the important hydrocarbon reservoir in southwest of Iran. In this research the Sarvak Formation with Cenomanian age has been investigated in some wells in Azadegan oil field in the north of the Dezful Embayment in south west Iran. This research has been focused on facies analysis, depositional environments and diagenetic processes in the Sarvak Formation. The thickness of the Sarvak Formation is varied from 608 to 637.5 meters in Azadegan wells. In these wells the Sarvak Formation is overlai n by the Ilam Formation uncomfortably. It is underlain the Kazhdumi Formation with conformable contact. Based on detail sedimentological analysis over the Sarvak formation four facies associations including tidal flat, lagoon, barrier and open marine have been recognized. The detailed microfacies analysis and sedimentological criteria suggest the Sarvak was deposited in rimmed shelf carbonate setting. The most important diagenetic processes include dolomitization, calcitization, cementation, pyritization, micritization, neomorphism, compaction, dissolution and biotorbation influenced Sarvak. From the petrophysical point of view, the porosity is the most important diagenetic process in the Sarvak Formation and fracture, vuggy and moldic types are dominant porosity types in this Formation." @default.
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• W2181433680 date "2010-01-01" @default.
• W2181433680 modified "2023-09-24" @default.
• W2181433680 title "Facies Analysis, Depositional Environments and Diagenesis of the Sarvak Formation in Azadegan Oil Field" @default.
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