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Micromorphology and formation mechanism of pisoliths in the Dehdasht bauxite deposits
The Dehdasht bauxite deposits are located 40 km northeast of Dehdasht in Kohgilouye and Boyer-Ahmad Province. It is a part of the Irano-Hymalayan karstic bauxite belt located in the upper part of karstic depressions of Santonian-Turonian Sarvak carbonate
Ali Reza Zarasvandi +4 more
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Caracterización del espacio poroso en el reservorio siliclástico y carbonatado de Kazhdumi, en un campo petrolífero en la llanura de Abadan, Irán [PDF]
Spatial porosity modeling is vital in static modeling, as variations in both lateral and vertical dimensions significantly influence reservoir quality and volumetric calculations.
Mehdipour, Vali, Sadeghtabaghi, Zahra
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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
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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 +2 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 +2 more
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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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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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Natural Resources Research, 2016
Introducing and applying an appropriate strategy for reservoir modeling in strongly heterogeneous and fractured reservoirs is a controversial issue in reservoir engineering. Various integration approaches have been introduced to combine different sources of information and model building techniques to handle heterogeneity in geological complex ...
Mehrdad Soleimani +2 more
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Introducing and applying an appropriate strategy for reservoir modeling in strongly heterogeneous and fractured reservoirs is a controversial issue in reservoir engineering. Various integration approaches have been introduced to combine different sources of information and model building techniques to handle heterogeneity in geological complex ...
Mehrdad Soleimani +2 more
openaire +1 more source

