Geochemistry, petrography, and tectono-magmatic setting of Eocene volcanic lavas in the south of Mamoniyeh, Urumieh-Dokhtar magmatic arc, Markazi Province, Iran [PDF]
پترولوژیThe study area lies in the south of Mamoniyeh, a part of the Zaviyeh 1:100000 geological map, which covers the middle part of the Urumieh-Dokhtar magmatic arc.
Mohammad Goudarzi +2 more
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Evaluation of Cu-mineralization potential based on mineralogical and geochemical evidence in Kahdelan area, Eastern Azerbaijan, NW of Iran [PDF]
پترولوژی, 2022 The Kahdelan area in the SW of Sarab is situated in the northern part of the Urumieh–Dokhtar geotectonic zone and Tarom-Hashtjin metallogenic zone. Some of the most important porphyry Cu ± Mo ± Au mineralizations in Iran occur along the NW–SE trending ...
Reyhane Lotfi +3 more
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Studies on genesis of chromite and PGE in Naein ophiolite melange
Journal of Economic Geology, 2012 Nain ophiolite melange is located 140 Km east of Isfahan. Based on the geological studies, this area belongs to Mesozoic ophiolite of Urumieh – Dokhtar zone, west of central Iran. Country rocks are pridotite and serpentinized pridotite.
Reza Shamsipour Dehkordi +2 more
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Investigation of the geochemical and mineralogical characteristics of the dikes associated with copper mineralization at the southeastern Ardestan (NE Isfahan) [PDF]
پترولوژی, 2017 The Ardestan study area lies in the northeast of Isfahan and at the outer margin of Urumieh -Dokhtar Volcanic Arc (UDMA). In this area, copper mineralization is associated with dikes.
Maryam Salehi +2 more
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Journal of Petrology, 2022 Abstract The Cenozoic Arabia–Iran continental collision was associated with emplacement of a large variety of magmatic rock types. This aspect is particularly evident in the Bijar-Qorveh area of NW Iran, where Miocene andesitic to rhyolitic rocks and Quaternary basic alkaline rocks crop out. The Miocene intermediate to acid products show
Fedele, L. +5 more
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Journal of Economic Geology, 2010 Sakhtehesar mountain is located in Urumieh-Dokhtar magmatic belt and is composed of volcanic and subvolcanic rocks (Pliocene andesite to dacite) which intruded the volcanics and pyroclastics of Paleocene age.
Farimah Ayati, Saeed Mahdevari
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Geochemistry and petrogenesis of the Dehe Bala calc-alkaline granodiorites, south west of Boein Zahra [PDF]
پترولوژی, 2016 The Dehe Bala pluton is exposed approximately 45 km south-west of Boein Zahra town, Qazvin province. This Pluton which intruded the Eocene volcano-sedimentary rocks of the Urumieh-Dokhtar Magmatic assemblage (UDMA), is mainly composed of granodiorite and
Zeynab Gharamohammadi, Ali Kananian
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Journal of Economic Geology, 2021 Introduction The studied area is situated 15 km away from the southwest of Maimeh at the western part of Urumieh-Dokhtar magmatic arc. This zone is a part of the Zagros orogenic belt formed due to the subduction of the Neo-Tethyan oceanic crust under ...
Shahzad Sherafat, Zahra Heidari Fetrat
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Petrology and geochemistry of igneous rocks and their relationship with mineralization in Talahoueieh area, north of Bam, Urumieh-Dokhtar Magmatic Arc [PDF]
پترولوژیIntroduction The Central Iran zone represents one of the most significant geological domains of Iran, characterized by a wide diversity of igneous, metamorphic, and sedimentary rocks formed through prolonged tectonic and magmatic processes.
Jalal Hassanshahi +2 more
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Alteration Mapping in Central Urumieh-Dokhtar Magmatic Assemblage of Iran Using ASTER and OLI Data
Open Journal of Geology, 2017 The study area is located on the Urumieh-Dokhtar Magmatic Assemblage of Iran, in the west of Ardestan between the East longitude 52°1' to 52°18' and the North latitude 33°17' to 33°27'. Remote sensing techniques are suitable for studying the alterations occurring in the igneous terranes.
Farshad Khodadadi, Ramin Arfania
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