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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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Deformation Mechanisms of Darreh Sary Metapelites, Sanandaj‒Sirjan Zone, Iran

Geotectonics, 2018
The Darreh Sary metapelitic rocks are located in the northeast of Zagros orogenic belt and Sanandaj-Sirjan structural zone. The lithological composition of these rocks includes slate, phyllite, muscovitebiotite schist, garnet schist, staurolite-garnet schist and staurolite schist.
O. Hemmati   +2 more
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Structural and metamorphic evolution of the southern Sanandaj-Sirjan zone, southern Iran

International Journal of Earth Sciences, 2022
The southern Sanandaj-Sirjan Zone (SSZ) forms the core of the Zagros orogen and consists of a stack of four major tectonic units, all of which were thrust southwestward over the Neyriz ophiolites. Precambrian and early Paleozoic rocks were affected by high-grade metamorphism, whilst the late Paleozoic (Carboniferous and Permian) and Mesozoic rocks are ...
Gharibnejad, Parisa   +4 more
openaire   +1 more source

A new tectonic scenario for the Sanandaj–Sirjan Zone (Iran)

Journal of Asian Earth Sciences, 2006
Abstract Recent geochemical studies of volcanic rocks forming part of the ophiolites within the Zagros and Naien-Baft orogen indicate that most of them were developed as supra-subduction ophiolites in intra-oceanic island arc environments. Intra-oceanic island arcs and ophiolites now forming the Naien-Baft zone were emplaced southwestward onto the ...
A. Ghasemi, C.J. Talbot
openaire   +1 more source

Documentation of the Sirjan Orocline in the southeast Sanandaj-Sirjan Zone, Iran

Journal of Mountain Science, 2020
At the southeastern part of the Sanandaj-Sirjan Zone of Iran, a group of structural elements outline a large-scale arc curvature around a vertical axis. This curvature comprises several elongated structural elements and their dividing faults, axialfold traces, layering, and foliation.
Abdolreza Partabian   +3 more
openaire   +1 more source

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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Cretaceous subduction-related volcanism in the northern Sanandaj-Sirjan Zone, Iran

Journal of Geodynamics, 2008
Cretaceous volcanic rocks (SCV) are widely developed in the northern part of the Sanandaj-Sirjan Zone, northwest Iran. Based on the mineralogy, texture and geochemical composition these rocks are divided in two main groups, the first and main one situated in the central part of the study area and the second one in the northeast.
Hossein Azizi, Ahmad Jahangiri
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Cretaceous–Tertiary convergence and continental collision, Sanandaj–Sirjan Zone, western Iran

Journal of Asian Earth Sciences, 2003
Abstract The Sanandaj–Sirjan Zone contains the metamorphic core of the Zagros continental collision zone in western Iran. The zone has been subdivided into the following from southwest to northeast: an outer belt of imbricate thrust slices (radiolarite, Bisotun, ophiolite and marginal sub-zones, which consist of Mesozoic deep-marine sediments ...
M Mohajjel, C.L Fergusson, M.R Sahandi
openaire   +1 more source

Saqez–Sardasht Goldfield, North Sanandaj‐Sirjan Zone, Iran: A Tectono‐Metallogenic Synthesis

Acta Geologica Sinica - English Edition, 2020
AbstractThe Sanandaj–Sirjan Zone (SSZ), as the metamorphic‐magmatic core of the Zagros Orogen in southwestern Iran, contains several styles of gold deposit of Phanerozoic age. The northern SSZ includes an ENE‐trending goldfield belt. This area that encompasses the main orogenic gold deposits, e.g., Qolqoleh, Kervian, Qabaqhlujeh, and the Barika VMS ...
Erfan HAJI   +3 more
openaire   +1 more source

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
openaire   +1 more source

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