Results 101 to 110 of about 149 (121)
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Proceedings, 2009
Spectacular outcrops of dolomite of hydrothermal origin are described from the Anaran Anticline, in the Simply Folded Belt of the Zagros Mountains, Ilam province, SW Iran. Dolomite replaces Cretaceous carbonates of the Upper and Lower Sarvak formation (Albian to Turonian).
F. Lapponi +6 more
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Spectacular outcrops of dolomite of hydrothermal origin are described from the Anaran Anticline, in the Simply Folded Belt of the Zagros Mountains, Ilam province, SW Iran. Dolomite replaces Cretaceous carbonates of the Upper and Lower Sarvak formation (Albian to Turonian).
F. Lapponi +6 more
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Carbonates and Evaporites, 2020
Static reservoir modeling for optimizing the strategies of hydrocarbon field developments using seismic data and well logs is the focus of this study. The static reservoir modeling is conducted to estimate reservoir properties of the Upper Sarvak formation in one of the offshore oil fields in the Persian Gulf.
Mehran Rahimi, Mohamad Ali Riahi
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Static reservoir modeling for optimizing the strategies of hydrocarbon field developments using seismic data and well logs is the focus of this study. The static reservoir modeling is conducted to estimate reservoir properties of the Upper Sarvak formation in one of the offshore oil fields in the Persian Gulf.
Mehran Rahimi, Mohamad Ali Riahi
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Journal of Petroleum Science and Engineering, 2022
Abstract Located in the northeast of the Arabian Plate, Zagros Basin hosts some of the most significant hydrocarbon reservoirs in Iran, including the Sarvak Formation. It has been dated back to the Middle Cretaceous and exhibits a dominantly carbonate lithology. In this study, petrographic and petrophysical data of the Sarvak Formation were analyzed.
Arad Kiani +3 more
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Abstract Located in the northeast of the Arabian Plate, Zagros Basin hosts some of the most significant hydrocarbon reservoirs in Iran, including the Sarvak Formation. It has been dated back to the Middle Cretaceous and exhibits a dominantly carbonate lithology. In this study, petrographic and petrophysical data of the Sarvak Formation were analyzed.
Arad Kiani +3 more
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Facies, 2015
The Sarvak reservoirs are characterized by thick rudist-dominated intervals in the south and southwest Iran. During the middle Cretaceous, rudistid communities were widely developed on the shallow parts of the Sarvak platform, mainly in the central Zagros and eastern Persian Gulf.
Behrooz Esrafili-Dizaji +5 more
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The Sarvak reservoirs are characterized by thick rudist-dominated intervals in the south and southwest Iran. During the middle Cretaceous, rudistid communities were widely developed on the shallow parts of the Sarvak platform, mainly in the central Zagros and eastern Persian Gulf.
Behrooz Esrafili-Dizaji +5 more
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2021
In this study, two stratigraphic sections of Sarvak Formation were selected which are nominated Bavan and Kherameh sections. Over 379.5 meters of the Sarvak Formation and 260 thin sections have been studied. Index microfacies and foraminifers have been identified. Index microfacies include Boundstone, Wackestone and Packstone. The frequency of bioclast
Massih Afghah, Hamid Reza Fadaei
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In this study, two stratigraphic sections of Sarvak Formation were selected which are nominated Bavan and Kherameh sections. Over 379.5 meters of the Sarvak Formation and 260 thin sections have been studied. Index microfacies and foraminifers have been identified. Index microfacies include Boundstone, Wackestone and Packstone. The frequency of bioclast
Massih Afghah, Hamid Reza Fadaei
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Marine and Petroleum Geology, 2020
Abstract Two surface sections of the Sarvak Formation (late Albian-late Turonian) named Tange-e Bawlek and Shahnakhjir were studied., These sections are about 24 km apart, located in the flanks of the Kabirkuh and Shahnakhjir anticlines in Ilam province, in the western part of the Zagros Fold Thrust Belt (ZFTB).
Hassan Mohseni +1 more
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Abstract Two surface sections of the Sarvak Formation (late Albian-late Turonian) named Tange-e Bawlek and Shahnakhjir were studied., These sections are about 24 km apart, located in the flanks of the Kabirkuh and Shahnakhjir anticlines in Ilam province, in the western part of the Zagros Fold Thrust Belt (ZFTB).
Hassan Mohseni +1 more
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Nigeria Annual International Conference and Exhibition, 2012
Abstract Ilam and Sarvak formations are two main Upper Cretaceous oil-bearing carbonate systems that are formed in an unconformity manner in Abadan plain, south-western Iran. Based on comprehensive geological and stratigraphic studies, eight reservoir zones are determined in these formations that four of them are major oil reservoirs ...
M. B Shahvar, R. Kharrat
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Abstract Ilam and Sarvak formations are two main Upper Cretaceous oil-bearing carbonate systems that are formed in an unconformity manner in Abadan plain, south-western Iran. Based on comprehensive geological and stratigraphic studies, eight reservoir zones are determined in these formations that four of them are major oil reservoirs ...
M. B Shahvar, R. Kharrat
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IOR 2007 - 14th European Symposium on Improved Oil Recovery, 2007
P01 Integrated 3D Seismic Petrophysical Data of the Sarvak Formation Sirri District in the Persian Gulf A. Bashari* (Irannian Offshore Oil Company) SUMMARY Sirri district forms part of vast sedimentary area located between: The Qatar uplift in the west. The mio-geosyncline of the Zagross in the north. The Omanides geosyncline in the south east.
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P01 Integrated 3D Seismic Petrophysical Data of the Sarvak Formation Sirri District in the Persian Gulf A. Bashari* (Irannian Offshore Oil Company) SUMMARY Sirri district forms part of vast sedimentary area located between: The Qatar uplift in the west. The mio-geosyncline of the Zagross in the north. The Omanides geosyncline in the south east.
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Micropaleontology, 2018
Microbiostratigraphy, microfacies and depositional environments of the Sarvak and Ilam formations have been studied in the Gachsaran Oilfield (well no. 335). The thickness of the Sarvak and Ilam formations are 95.5 and 66.5 meters respectively and they consist of limestone with minor shale.
Mojgan Rikhtegarzadeh +4 more
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Microbiostratigraphy, microfacies and depositional environments of the Sarvak and Ilam formations have been studied in the Gachsaran Oilfield (well no. 335). The thickness of the Sarvak and Ilam formations are 95.5 and 66.5 meters respectively and they consist of limestone with minor shale.
Mojgan Rikhtegarzadeh +4 more
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Petroleum Science and Technology, 2014
Carbonate sequence of upper cretaceous (Cenomanian) of Sarvak Formation is a part of Bangestan Group with the thickness of 760m in Ahvaz oil field (well no. 63). This formation is overlain by the Kazhdumi Formation and is uncomfortably underlain by the Ilam Formation.
Asgari, M +2 more
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Carbonate sequence of upper cretaceous (Cenomanian) of Sarvak Formation is a part of Bangestan Group with the thickness of 760m in Ahvaz oil field (well no. 63). This formation is overlain by the Kazhdumi Formation and is uncomfortably underlain by the Ilam Formation.
Asgari, M +2 more
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