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A study of granite typology in Sanandaj-Sirjan zone, Zagros Orogen, Iran

Geochimica et Cosmochimica Acta, 2006
Department of Geology, Bu Ali Sina University, Hamadan andYoung Researchers Club of Kurdistan, IranEach granitoid type is generated and emplaced in every specifictectonic setting and each stage of the Wilson cycle is characterizedby typical associations of granitoids.
Ali A. Sepahi, Seyed F. Athari
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Metamorphism and deformation of golpayegan metapelitic rocks, Sanandaj-Sirjan Zone, Iran

Petrology, 2012
The metapelitic schists of the Golpayegan region can be divided into four groups based on their mineral assemblages: (1) garnet-chloritoid schists, (2) garnet schists, (3) garnet-staurolite schists, and (4) staurolite-kyanite schists. Paleozoic pelagic shales experienced progressive metamorphism and polymetamorphism from greenschist to amphibolite ...
S. Karimi   +3 more
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Episodic subduction initiation triggered Jurassic magmatism in the Sanandaj–Sirjan zone, Iran

Lithos, 2021
Abstract The Zagros suture zone in Iran is part of the Tethyan orogenic belt that records convergence between the Eurasian and Arabian plates during the Mesozoic-Cenozoic. Prior to collision, which may have initiated in the Late Eocene-Early Oligocene, much of the convergence was accommodated by the Late Triassic-Early Jurassic subduction of the ...
Reza Maghdour-Mashhour   +5 more
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Petrology of eclogites from north of Shahrekord, Sanandaj-Sirjan Zone, Iran

Mineralogy and Petrology, 2007
Metabasic rocks were recently found within a ductile shear zone in the north of Shahrekord, being a part of the structural zone of Sanandaj-Sirjan, SW Iran. The rocks give evidence of a so far unrecognized eclogite facies metamorphic event and testify to high pressure metamorphism in the Sanandaj-Sirjan Zone, near the Main Zagros Reverse Fault, which ...
A. R. Davoudian   +3 more
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Sedimentology and origin of Meyghan lake/playa deposits in Sanandaj–Sirjan zone, Iran

Carbonates and Evaporites, 2012
The inland lake/playa of Meyghan is a closed basin in the Sanandaj–Sirjan tectonic zone of Iran, containing largest mineable sodium sulfate deposit of the Middle East. The Late Pleistocene–Holocene sediments of this lake/playa were studied for sedimentological and mineralogical characteristics, brine evolution path and the record of climatic variations
Hossain Rahimpour-Bonab, Leila Abdi
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The continuation of the Kazerun fault system across the Sanandaj–Sirjan zone (Iran)

Journal of Asian Earth Sciences, 2009
Abstract The Kazerun (or Kazerun-Qatar) fault system is a north-trending dextral strike-slip fault zone in the Zagros mountain belt of Iran. It probably originated as a structure in the Panafrican basement. This fault system played an important role in the sedimentation and deformation of the Phanerozoic cover sequence and is still seismically active.
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Structure of the Soresat Metamorphic Complex, North Sanandaj–Sirjan Zone, northwest Iran

Australian Journal of Earth Sciences, 2009
The metasedimentary and granitoid rocks of the Soresat Metamorphic Complex occur along the northern margin of the Sanandaj–Sirjan Zone in northwest Iran. Four different deformational events (D1–D4) are recorded in the Soresat Metamorphic Complex.
A. Ghasemi, M. Poor Kermani
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Mesozoic magmatism in the northwestern Sanandaj–Sirjan zone as an evidence for active continental margin

Arabian Journal of Geosciences, 2014
The study area is northwest part of Sanandaj–Sirjan or Esfandegha–Marivan zone in the northwest of Iran. The oldest rocks which are limestone, sandstone, tuff, and lava belong to the Jurassic which have deformed during the Late Cimmerian orogeny. This complex is unconformably overlain by Cretaceous volcano sedimentary.
Hossein Moinevaziri   +2 more
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Deformations of Palaeozoic and Mesozoic Rocks in Southern Sirjan, Sanandaj–Sirjan Zone, Iran

Journal of Asian Earth Sciences, 2015
Abstract Structural and stratigraphic investigations in the southern part of the Sanandaj–Sirjan Zone, south of Sirjan indicate that the Palaeozoic and Mesozoic rocks have been affected by at least two syn-metamorphic regional deformations. The older regional deformation, known as the Early Cimmerian event, affected the Palaeozoic rocks and ...
exaly   +2 more sources

Petrogenesis of granitic unit of Naqadeh complex, Sanandaj–Sirjan Zone, NW Iran

Arabian Journal of Geosciences, 2009
The granitic unit is a component of the Naqadeh plutonic complex, NW of Sanandaj–Sirjan Zone (NW Iran). This unit is composed of high-K calc-alkaline, slightly peraluminous (ASI = 1.12–1.17) evolved monzogranites. These monzogranites have 41.85 ± 0.81 Ma (zircon U–Pb sensitive, high-resolution ion microprobe (SHRIMP) age) with two inherited zircon ages
Seyed Ali Mazhari   +3 more
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