Results 201 to 210 of about 713,265 (269)
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Geological Journal, 2022
The Tarbur Formation is a carbonate stratigraphic unit in the Zagros Basin. This formation is exposed between the Main Zagros Reverse and High Zagros faults and Sabzpoushan Fault.
Borzu Asgari-Pirbalouti, M. Dehghanian
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The Tarbur Formation is a carbonate stratigraphic unit in the Zagros Basin. This formation is exposed between the Main Zagros Reverse and High Zagros faults and Sabzpoushan Fault.
Borzu Asgari-Pirbalouti, M. Dehghanian
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SPE Journal
The heterogeneity indices in conventional carbonate reservoirs are usually influenced by various diagenetic processes. The main aim of this study is to build 3D geological models of the diagenetic and heterogeneity indices addressing the role of ...
Vali Mehdipour +2 more
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The heterogeneity indices in conventional carbonate reservoirs are usually influenced by various diagenetic processes. The main aim of this study is to build 3D geological models of the diagenetic and heterogeneity indices addressing the role of ...
Vali Mehdipour +2 more
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Geological Journal
The shallow marine carbonate deposits of the Sarvak Formation have been deposited in an active tectonic setting under warm and humid climatic conditions during the Cenomanian–Turonian (C–T).
Emad Yahyaei, H. Mehrabi, Ramin Abbasi
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The shallow marine carbonate deposits of the Sarvak Formation have been deposited in an active tectonic setting under warm and humid climatic conditions during the Cenomanian–Turonian (C–T).
Emad Yahyaei, H. Mehrabi, Ramin Abbasi
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Biostratigraphy and Paleoecology of Maastrichtian Sediments in the Zagros Basin, Iran
Acta Geologica Sinica - English Edition, 2013Abstract:To enable the lithostratigraphic and biostratigraphic study of the Gurpi Formation, within the ‘Dezak’ or Globigerina Marl, a stratigraphic section at Booraki, located to the NNW of Shiraz, SW Iran, through the late Cretaceous was examined.
Mahnaz Parvaneh Nejad SHIRAZI +2 more
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PERMIAN AND TRIASSIC STRATIGRAPHY, ZAGROS BASIN, SOUTH‐WEST IRAN
Journal of Petroleum Geology, 1978The Permian and Triassic beds deposited in the Zagros Basin form a massive carbonate and evaporite sequence in excess of 2000m. These strata were divided into clearly recognizable and mappable lithostratigraphic units and major lithofacies types using surface exposures, subsurface log information and sample cuttings.
Frank Szabo, Ahmad Kheradpir
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Tectonophysics, 2008
The regionally extensive, coarse-grained Bakhtiyari Formation represents the youngest synorogenic fill in the Zagros foreland basin of Iran. The Bakhtiyari is present throughout the Zagros fold-thrust belt and consists of conglomerate with subordinate sandstone and marl.
Fakhari, Mohammad D. +4 more
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The regionally extensive, coarse-grained Bakhtiyari Formation represents the youngest synorogenic fill in the Zagros foreland basin of Iran. The Bakhtiyari is present throughout the Zagros fold-thrust belt and consists of conglomerate with subordinate sandstone and marl.
Fakhari, Mohammad D. +4 more
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Palynostratigraphy of Devonian sediments in the Zagros Basin, southern Iran
Review of Palaeobotany and Palynology, 2003Abstract A total of 100 surface samples from the Zakeen and Faraghan formations were collected and processed in the palynological laboratory of the Exploration Directorate of the National Iranian Oil Company. The majority of surface samples contain well-preserved and abundant palynomorph taxa (acritarchs, miospores and scolecodonts).
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Geological Journal, 2022
In this manuscript, Notes to comment on “Evolutionary trend of Cenomanian alveolinids from Zagros Basin, SW of Iran” by Consorti and Vicedo (2022) in Geological Journal, will be answered.
Mahtab Dousti Mohajer +3 more
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In this manuscript, Notes to comment on “Evolutionary trend of Cenomanian alveolinids from Zagros Basin, SW of Iran” by Consorti and Vicedo (2022) in Geological Journal, will be answered.
Mahtab Dousti Mohajer +3 more
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Distribution of Miogypsinoides in the Zagros Basin, in southwest Iran
Historical Biology, 2008In the present study three species of Miogypsinoides are described from the Oligocene–Miocene Asmari Formation of the Zagros Basin in the southwest of Iran. This is the explanation of the morphological recognition and distribution of Miogypsinoides complanatus, Miogypsinoides formosensis (Upper Oligocene, Chattian) and Miogypsinoides dehaartii (Lower ...
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