Mineral chemistry, tectonic setting and thermo-barometry of the gabbro-diorite intrusive body (south of Tikmehdash), East-Azarbaijan
Mineral chemistry, tectonic setting and thermo-barometry of the gabbro-diorite intrusive body (south of Tikmehdash), East-Azarbaijan

Marzieh Rezaeiaghdamََ; Ahmad Jahangiri; Mohsen Moayyed; Ghahraman Sohrabi

Volume 13, Issue 1 , August 2022, , Pages 117-142

https://doi.org/10.22108/ijp.2020.122066.1168

Abstract
  The Bostanabad-Hashtrood gabbro-diorite intrusive body in the south of Tikmehdash has intruded the Eocene volcanic-sedimentary rocks. The chemistry of the constituent minerals in this ...  Read More
Magma source and the evolution of Early Paleozoic (Silurian) metavolcanic rocks of Maku area (northwest of Iran):
An evidence for Paleotethys drifting
Magma source and the evolution of Early Paleozoic (Silurian) metavolcanic rocks of Maku area (northwest of Iran): An evidence for Paleotethys drifting

Farzaneh Valinasab Zarnagh; Mohsen Moayyed; Ahmad Jahangiri; Haji Hossein Azizi

Volume 12, Issue 1 , June 2021, , Pages 19-40

https://doi.org/10.22108/ijp.2020.121834.1166

Abstract
  A vast part of the Central Iranian and Alborz zones have affected by an extensional tectonic regime in the lower Paleozoic, especially the Silurian period. Due to some clear relation ...  Read More
Garmichay S-type granites (northwestern Iran):
Whole rock geochemistry, tectonic setting
and generation mechanism
Garmichay S-type granites (northwestern Iran): Whole rock geochemistry, tectonic setting and generation mechanism

Amir Mahamed; Mohsen Moayyed; Monir Modjjarad

Volume 11, Issue 1 , May 2020, , Pages 53-72

https://doi.org/10.22108/ijp.2019.118558.1146

Abstract
  The Garmichay area in the north of Mianeh, NW Iran, features schists, amphibolites, calc-silicates, marbles and granitoids. Granitoids are of S- and A-type nature. Partial melting is ...  Read More
Geochemistry and petrogenesis of Alamdar rhyolites
from East of Tasouj town (Northwest of Iran)
Geochemistry and petrogenesis of Alamdar rhyolites from East of Tasouj town (Northwest of Iran)

Mohsen Moayyed; Robab Hajialioghli

Volume 9, Issue 2 , September 2018, , Pages 21-38

https://doi.org/10.22108/ijp.2018.81989.0

Abstract
  The Alamdar rhyolite has been cropped out at the highest top of Mishow Mountain Ranges (i.e. Alamdar top), east of Tasouj. Considering that the rhyolite has been intruded the Kahar ...  Read More
An Introduction to camptonite lamprophyric dikes at Misho Mountains (Almas area - East Azarbaijan Province)
An Introduction to camptonite lamprophyric dikes at Misho Mountains (Almas area - East Azarbaijan Province)

Mohsen moayyed; zahra Gharehchahi; jamshid Ahmadiyan; Mamuru Murata; Peyman Ghasemi

Volume 8, Issue 30 , September 2017, , Pages 119-138

https://doi.org/10.22108/ijp.2017.82003

Abstract
  The Almas area in NW of the East Azarbaijan Province, is a part of the Soltaniye-Misho zone. The lamprophyric dikes crosscut the Kahar Formation. The principal minerals of these rocks ...  Read More
Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)
Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)

Saeed Kamran; Ahmad Jahangiri; Robab Hajialioghli; Mohsen Moayyed

Volume 8, Issue 29 , June 2017, , Pages 37-52

https://doi.org/10.22108/ijp.2017.21499

Abstract
  The investigated granite intrusion is located at the north of Ayghalesi village, east of Takab The Ayghalesi granite has been intruded the Eocene sandstone and conglomerate rocks and ...  Read More
Rb/Sr and Sm/Nd isotope geochemistry and petrogenesis of Mishu granitoid rocks, northwest of Iran
Rb/Sr and Sm/Nd isotope geochemistry and petrogenesis of Mishu granitoid rocks, northwest of Iran

Malihe Shahzeidi; Mohsen Moayyed

Volume 6, Issue 24 , January 2016, , Pages 87-114

Abstract
  The Mishu granitoids occur in northwest of Central Iran and are part of the Khoy-Takab Precambrian metamorphic belt. Based on petrographic studies, this complex comprises several intrusions ...  Read More
Mineral chemistry and petrology of lamprophyric dyke in Guyposhti Mountain (northwest Maragheh-East Azarbaijan)
Mineral chemistry and petrology of lamprophyric dyke in Guyposhti Mountain (northwest Maragheh-East Azarbaijan)

Mousa Akbarzadeh Laleh; Nasir Amel; Mohsen Moayyed; Ahmad Jahangiri

Volume 6, Issue 24 , January 2016, , Pages 115-130

Abstract
  The study area is located about 30 km northwest of Maragheh in East Azerbaijan. The lamprophyric dyke intruded the Shemshak sedimentary rocks. Based on stratigraphic evidences, the ...  Read More
Petrogenesis of adakitic Plio-Quaternary post collision rocks, north of Sahand volcano (NW of Iran)
Petrogenesis of adakitic Plio-Quaternary post collision rocks, north of Sahand volcano (NW of Iran)

Nasir Amel; Vahideh Jalili Ghareh Ghaye; Robab Hajialioghli; Mohsen Moayyed

Volume 6, Issue 22 , July 2015, , Pages 157-172

Abstract
  The study area is situated in the south of Sahand volcano in the northwest of Iran. The volcanic rocks in this area are part of young activity of Sahand volcano, erupted as flow lavas ...  Read More
Petrography and petrology of the Sungun porphyry copper deposit and post mineralization dykes with a view to Skarn mineralization (north of Varzeghan, East Azarbaijan)
Petrography and petrology of the Sungun porphyry copper deposit and post mineralization dykes with a view to Skarn mineralization (north of Varzeghan, East Azarbaijan)

Mohamad Reza Hosseinzadeh; Seyed Ghafour Alavi; Mohsen Moayyed

Volume 5, Issue 17 , April 2014, , Pages 17-32

Abstract
  The Sungun porphyry copper mine is located in the north of Varzeghan, Eastern- Azarbaijan province. The oldest rocks in the study area are limestone with the Cretaceous in age. Following ...  Read More
Study cause of tertrad effect in REE pattern in Misho A-type granitoides Complex, NW of Iran
Study cause of tertrad effect in REE pattern in Misho A-type granitoides Complex, NW of Iran

Maryam Ahankoub; Ahmad Jahangiri; Mohsen Moayyed

Volume 3, Issue 10 , December 2012, , Pages 65-78

Abstract
  A-Type granitoides of the East Misho, are per-aluminous to sub-aluminous rocks that formed by partial melting of lower crustal rocks. Their essential composed of quartz, K-Feldspar, ...  Read More
Geology and geochemistry of Mishu S-type granitoid NW Iran
Geology and geochemistry of Mishu S-type granitoid NW Iran

Maliheh Shahzeidi; Mohsen Moayyed; Shoji Arai; Tahmineh Pirnia; Jamshid Ahmadian

Volume 3, Issue 11 , December 2012, , Pages 111-126

Abstract
  The Mishu garnitoid complex, located NW of Mishu Mountains, southwest of Marand and northwest of Iran (East Azarbaidjan), and intruded into the metamorphosed Precambrian rocks (Kahar ...  Read More
The petrography and geochemistry of volcanic rocks of Ghaflankuh, Myaneh (NW Iran)
The petrography and geochemistry of volcanic rocks of Ghaflankuh, Myaneh (NW Iran)

Amin Allah Kamali; Mohssen Moayyed; Ahmad Jahangiri; Nasir Amel; Hadi Pirooj; Ali Ameri

Volume 2, Issue 6 , November 2011, , Pages 97-115

Abstract
  The study area is a part of the western Alborz-Azarbaijan magmatic belt. The main outcrops in Ghaflankuh are including alternative andesite lava, andesite-basalt, trachy-andesite and ...  Read More
Whole rock chemistry of Shahindezh metapelites, provenance and mineral parageneses
Whole rock chemistry of Shahindezh metapelites, provenance and mineral parageneses

Monir Modjarrad; Mohsen Moazzen; Mohsen Moayyed

Volume 1, Issue 4 , March 2011, , Pages 73-88

Abstract
  In order to identify the provenance of metasediments of the Shahindezh Metamorphic Complex (SMC), NW Iran, we have studied the bulk chemistry of the metapelites in the mentioned area. ...  Read More
The study of geochemical characteristics of Natanz plutonic complex, North of Isfahan
The study of geochemical characteristics of Natanz plutonic complex, North of Isfahan

Maryam Honarmand; Mohsen Moayyed; Ahmad Jahangiri; Jamshid Ahmadian; Noushin Bahadoran

Volume 1, Issue 3 , December 2010, , Pages 65-88

Abstract
  The Natanz plutonic complex is located 120 km north of Isfahan and in the Orumieh - Dokhtar magmatic belt. These Oligocene - Miocene plutons are intruded into the volcanics of Eocene. ...  Read More
Introducing the Ghorveh fibrolites and their formation condition
Introducing the Ghorveh fibrolites and their formation condition

Hadi Omrani; Mohsen Moayyed; Ahmad Jahangiri; Mohsen Moazzen

Volume 1, Issue 1 , June 2010, , Pages 1-10

Abstract
  The metamorphic rocks of the Ghorveh area, southeast of Sanandaj, are classified as a part of the Sanandaj-Sirjan metamorphic zone. South of Ghorveh includes an assemblage of regional ...  Read More