Results 211 to 220 of about 713,265 (269)
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Biostratigraphic Revision of Middle-Cretaceous Biostratigraphy Succession in South Zagros Basin
Journal of Earth Science & Climatic Change, 2014Cenomanian succession (Sarvak Formation) is well distributed along Zagros area particularly in the south portion of the Zagros (Fars area). This study attempts to determine the precise biostratigraphic biozones of four stratigraphic sections selected from the Cenomanian strata south Zagros basin, including the sections of Nour Abad, Samghan, Doroodzan,
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Petroleum source-rock potential of the Piranj oil field, Zagros basin
Marine and Petroleum Geology, 2016Abstract Zagros basin constitutes one of the most prolific hydrocarbon producing habitats and the second largest basin in the Middle East. The Piranj oil field is part of The Middle Cretaceous–Early Miocene Petroleum System in Zagros basin and southwest of Iran.
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Sequence Stratigraphy of Pabdeh Formation in Dezful Embayment (Zagros Basin) SW Iran
GEO 2010, 2010Pabdeh Formation (upper Eocene-Oligocene) is a carbonate dominated sedimentary package with shale -marl intervals. This Formation was studied the type section (Kuh-E-Gurpi) and four boreholes located in Dezful Embayment (Zagros Basin). The Pabdeh Formation comprises three depositional sequences bounded by Type I sequence boundary in lower part and both
Mehdi Khoshnoodkia +2 more
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Tectono-sedimentary framework of the Gachsaran Formation in the Zagros foreland basin
Marine and Petroleum Geology, 2004Abstract Continental collision between Iranian and Arabian plates resulted in the formation of the Zagros fold–thrust belt and its associated foreland basin. During convergence, pre-existing faults in the basement were reactivated and the sedimentary cover was shortened above two different types of basal decollement (viscous/frictional).
Abbas Bahroudi, Hemin A. Koyi
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Subsidence history of the Middle East Zagros Basin, Permian to Recent
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1982The Zagros Basin is broadly defined as the palaeodepositional wedge of sediments along the present belt of the Zagros Mountains. A series of ten regional isopach maps trace the development of a portion of this basin from Permian to Recent. From the Permian to the middle Cretaceous the area occupied a position along the stable northeastern Atlantic-type
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Controls on the sequence stratigraphic architecture of the Neogene Zagros foreland basin
2018We investigated the sequence stratigraphic architecture of Neogene deposits in the Zagros region using 12 measured stratigraphic sections and performing strontium isotope measurements on 10 samples. We combined our data with 44 previous published Sr isotope measurements and fi ve paleomagnetostratigraphic sections in order to place the foreland ...
Pirouz, Mortaza +4 more
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Barremian-Aptian Calcareous Nannofossil Biostratigraphy in Zagros Basin (west Iran), Tethyan Realm
Stratigraphy and Geological Correlation, 2018The calcareous nannofossils from the upper part of Garau Formation were studied in the NW Zagros Basin, western Iran (Kabir-Kuh section). The ca. 510 m thick studied interval is mainly composed of interlayered marls, marly limestones, marly shales, laminated black shales and limestones.
A. Mahanipour +2 more
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Paleoecology & Paleobiogeography of Orbitoides Genus in Zagros Basin (South West Iran)
Journal of Earth Science & Climatic Change, 2015Orbitoides is a large size benthic foraminifera of Tarbur Foarmation (Late Campanian -Maastrichtian) distributed from Northwest to southeast of Zagros area. From the Paleoenvironment point of view this genus lives in shallow environment with high aggitation, high light penetration and low clastic particles in let (like reefs and barrier reefs).
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Journal of Earth Science, 2014
The Sachun Formation in the Zagros Mountains Ranges was sampled on the basis of changes in lithology and 150 vertically oriented thin-sections were prepared and subjected to detailed petrographic study. Evaporite, carbonate and shale/marl facies are identified here.
Solmaz Arzaghi, Massih Afghah
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The Sachun Formation in the Zagros Mountains Ranges was sampled on the basis of changes in lithology and 150 vertically oriented thin-sections were prepared and subjected to detailed petrographic study. Evaporite, carbonate and shale/marl facies are identified here.
Solmaz Arzaghi, Massih Afghah
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Journal of Asian Earth Sciences, 2019
Abstract The Zaribar Lake is situated along the Main Recent Fault, a dextral major strike-slip active fault system in the Zagros collision zone. The formation of the Zaribar Lake in Late Pleistocene is associated with the activities of the Main Zagros Reverse Fault, initiated in Late Oligocene, and with the Main Recent Fault, whose inception occurred
Bahman Rahimzadeh +4 more
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Abstract The Zaribar Lake is situated along the Main Recent Fault, a dextral major strike-slip active fault system in the Zagros collision zone. The formation of the Zaribar Lake in Late Pleistocene is associated with the activities of the Main Zagros Reverse Fault, initiated in Late Oligocene, and with the Main Recent Fault, whose inception occurred
Bahman Rahimzadeh +4 more
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