Results 111 to 120 of about 273 (153)
Integrating optimization and machine learning for estimating water resistivity and saturation in shaley sand reservoirs. [PDF]
Sci RepHameedy MAE, Mabrouk WM, Metwally AM.
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Reservoir characterization of Sarvak Formation from velocity deviation log and cutting sample studies, Dezful Embayment, Iran [PDF]
, 2008 Rashel Mostafaee, Faeze M. Tabesh
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Development of a new hydraulic electric index for rock typing in carbonate reservoirs. [PDF]
Sci RepMohammadi M +4 more
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Original Mineralogy and Recognition of Upper Boundary of the Sarvak Formation Based on Geochemistry and Isotope Studies [PDF]
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.
A Barari
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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
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 +2 more
exaly +2 more sources
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 +2 more
exaly +2 more sources
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 +2 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 +2 more sources
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
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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
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, Honarmand Javad
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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, Honarmand Javad
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Organic Geochemistry, 2016
Cenomanian Middle Sarvak rock samples were collected from various parts of the eastern Iranian sector of the Persian Gulf and analyzed for quantity, quality, maturity and depositional environment of the organic matter by Rock–Eval pyrolysis, gas chromatography (GC), gas chromatography–mass spectrometry (GC–MS), pyrolysis–gas chromatography–mass ...
Ehsan Hosseiny +2 more
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Cenomanian Middle Sarvak rock samples were collected from various parts of the eastern Iranian sector of the Persian Gulf and analyzed for quantity, quality, maturity and depositional environment of the organic matter by Rock–Eval pyrolysis, gas chromatography (GC), gas chromatography–mass spectrometry (GC–MS), pyrolysis–gas chromatography–mass ...
Ehsan Hosseiny +2 more
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