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Active strike-slip faulting in the Zagros Mountains: Geological and geomorphological evidence of the pull-apart Zaribar Lake basin, Zagros, NW Iran

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
Hossein Mahmoudi   +2 more
exaly   +2 more sources

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, 1982
Abstract The 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
W. J. Koop, R. Stoneley
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Palynostratigraphy of Devonian sediments in the Zagros Basin, southern Iran

Review of Palaeobotany and Palynology, 2003
Abstract 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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BASIN EVOLUTION OF THE LURESTAN REGION IN THE ZAGROS FOLD‐AND‐THRUST BELT, IRAN

Journal of Petroleum Geology, 2008
The evolution of the central part of the Lurestan region in the Zagros fold‐and‐thrust belt has been studied using newly generated isopach maps for different time intervals between the Late Cretaceous and the Miocene. The study was based on existing geological maps, gravity data, measured stratigraphic surface sections, original field work and well ...
A. Farzipour‐Saein   +3 more
openaire   +1 more source

Controls on the sequence stratigraphic architecture of the Neogene Zagros foreland basin

2018
We 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
openaire   +3 more sources

Biostratigraphy of the Kazhdumi Formation (Albian), northeast of Shiraz, Zagros Basin (SW of Iran)

Carbonates and Evaporites, 2020
The Kazhdumi Formation is one of the most significant rock units in the Bangestan Group in Zagros Basin. In this study, one section of the Kazhdumi Formation (Kuh-e-Rahmat) was selected for research. The section is extended approximately 89 m thick. The lower lithostratigraphic limit of the Kazhdumi Formation is marked by an oxidized zone, while the ...
Massih Afghah   +2 more
openaire   +1 more source

Neogene provenance evolution of the Zagros foreland basin: Implication for the uplift and outward growth history of the Zagros orogenic belt, Iran

Geological Society of America Bulletin
Abstract The Arabia-Eurasia convergence led to the uplift of the Zagros orogenic belt and the outward propagation of the fold-and-thrust system. In this paper we focus on the Miocene strata in southwestern Iran to study the stratigraphic chronology, basin evolution, and uplift history of the Iranian Plateau.
Jimin Sun   +7 more
openaire   +1 more source

Petroleum source-rock potential of the Piranj oil field, Zagros basin

Marine and Petroleum Geology, 2016
Abstract 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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Biostratigraphic Revision of Middle-Cretaceous Biostratigraphy Succession in South Zagros Basin

Journal of Earth Science & Climatic Change, 2014
Cenomanian 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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Investigating the Sediments of the Pabdeh Formation in Zagros Basin, Iran

2023 AAPG Rocky Mountain Section Meeting, 2023
Fatemeh Saberi, Mahboubeh Hosseini-Barzi
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