Results 121 to 130 of about 9,546,101 (182)
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Acta Geologica Sinica, 2021
AbstractThe Sarvak Formation is a carbonate sequence of Late Albian–Early Turonian age in Zagros Basin in Iran. In this investigation, the Sarvak Formation at the Pyun Anticline section (Izeh Zone) has been studied. It consists of 797 m thick limestone which overlies the Kazhdumi Formation conformably and underlies the Gurpi Formation unconformably at ...
Massih Afghah +1 more
exaly +3 more sources
AbstractThe Sarvak Formation is a carbonate sequence of Late Albian–Early Turonian age in Zagros Basin in Iran. In this investigation, the Sarvak Formation at the Pyun Anticline section (Izeh Zone) has been studied. It consists of 797 m thick limestone which overlies the Kazhdumi Formation conformably and underlies the Gurpi Formation unconformably at ...
Massih Afghah +1 more
exaly +3 more sources
Facies, 2016
The late Albian–early Turonian Sarvak Formation is the most important carbonate reservoir of the Abadan Plain, SW Iran. Twelve microfacies were identified, representing six facies belts: lagoon, shoal, rudist biostrome, slope, proximal, and distal open marine.
Javad Honarmand
exaly +3 more sources
The late Albian–early Turonian Sarvak Formation is the most important carbonate reservoir of the Abadan Plain, SW Iran. Twelve microfacies were identified, representing six facies belts: lagoon, shoal, rudist biostrome, slope, proximal, and distal open marine.
Javad Honarmand
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CHEMOSTRATIGRAPHY OF CENOMANIAN–TURONIAN CARBONATES OF THE SARVAK FORMATION, SOUTHERN IRAN
Journal of Petroleum Geology, 2012Stable‐isotope and trace‐element analyses from five surface and subsurface sections of the mid‐Cretaceous Sarvak Formation in southern and offshore Iran confirm the presence of the regional‐scale Turonian unconformity and of a more local Cenomanian–Turonian unconformity.
E. Hajikazemi +2 more
exaly +2 more sources
Depositional history of the uppermost Albian–Turonian Sarvak Formation in the Izeh Zone (SW Iran)
International Journal of Earth Sciences, 2021The uppermost Albian–Turonian interval has been studied in the south of the Izeh Zone (SW Iran) to investigate the depositional history of the Sarvak Formation in this area. This interval in the Middle East is characterized by the presence of very large shallow water carbonate platforms, surrounding the intra-shelf basins.
Behnaz Kalanat +2 more
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Carbonates and Evaporites, 2021
The Sarvak Formation is a thick carbonate sequence of Cenomanian age that has been deposited in a foreland basin across the Zagros Basin. Sarvak Formation is the main petroleum reservoir rock in the Zagros Basin. To study the foraminiferal paleoecology in the Sarvak Formation, the section was selected in the east of Shiraz (Khane Kat section) and 66 ...
Mohammadsadegh Dehghanian, Massih Afghah
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The Sarvak Formation is a thick carbonate sequence of Cenomanian age that has been deposited in a foreland basin across the Zagros Basin. Sarvak Formation is the main petroleum reservoir rock in the Zagros Basin. To study the foraminiferal paleoecology in the Sarvak Formation, the section was selected in the east of Shiraz (Khane Kat section) and 66 ...
Mohammadsadegh Dehghanian, Massih Afghah
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Sedimentary Geology, 2013
Abstract The Sarvak Formation (Albian to Cenomanian), forming part of the Bangestan Group, comprises a thick succession of carbonate rocks in the Zagros Basin of Southern Iran. The Sarvak Formation forms one of the main hydrocarbon reservoirs of this region. Three sections in the northern (252 m thickness) and southern flanks (348 m thickness) of the
Elham Asadi Mehmandosti +1 more
exaly +2 more sources
Abstract The Sarvak Formation (Albian to Cenomanian), forming part of the Bangestan Group, comprises a thick succession of carbonate rocks in the Zagros Basin of Southern Iran. The Sarvak Formation forms one of the main hydrocarbon reservoirs of this region. Three sections in the northern (252 m thickness) and southern flanks (348 m thickness) of the
Elham Asadi Mehmandosti +1 more
exaly +2 more sources
Marine and Petroleum Geology, 2020
The Albian–Turonian Sarvak Formation is the second most important reservoir of Iran. In this study, an integrated field-scale reservoir zonation is applied to the Sarvak reservoir in one oil field of the Dezful Embayment, SW Iran to understand the ...
Aram Bayet Goll, Mehdi Daraei
exaly +2 more sources
The Albian–Turonian Sarvak Formation is the second most important reservoir of Iran. In this study, an integrated field-scale reservoir zonation is applied to the Sarvak reservoir in one oil field of the Dezful Embayment, SW Iran to understand the ...
Aram Bayet Goll, Mehdi Daraei
exaly +2 more sources
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 African Earth Sciences, 2019
During Middle Cretaceous (Late Albian-Early Turonian) period, the Sarvak Formation prevailed in the coastal Fars area (Zagros), southern Iran. This formation is one of the main hydrocarbon reservoirs in the Zagros Basin which has gradually been deposited
Parisa Gholamizadeh +2 more
exaly +2 more sources
During Middle Cretaceous (Late Albian-Early Turonian) period, the Sarvak Formation prevailed in the coastal Fars area (Zagros), southern Iran. This formation is one of the main hydrocarbon reservoirs in the Zagros Basin which has gradually been deposited
Parisa Gholamizadeh +2 more
exaly +2 more sources