Stable isotope evidence for the genesis of Zn-Pb sulfide mineralization in the Kuh-e-Surmeh deposit
Stable isotope evidence for the genesis of Zn-Pb sulfide mineralization in the Kuh-e-Surmeh deposit

Batoul Taghipour; Safiyeh Eskandari

Volume 5, Issue 17 , April 2014, Pages 1-16

Abstract
  The Kuh-e-Surmeh Pb-Zn deposit is located 50 km south of Firouzabad in the Zagrous mountain folding belt. The upper Permian carbonates of lower Dalan Formation are hosted by mineralization. ...  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
Penetrative conditions and tectonomagmatic setting of the Takht granitic batholith, Sirjan
Penetrative conditions and tectonomagmatic setting of the Takht granitic batholith, Sirjan

Abdolnaser Fazlnia; Susan Jamei; Amin Jafari

Volume 5, Issue 17 , April 2014, Pages 33-50

Abstract
  The Takht granitic batholith of Sirjan contains gabbro-diorite to alkali-feldspar granite in composition. The batholith was emplaced in the south of the Urmia-Dokhtar magmatic belt ...  Read More
Petrology and geochemistry of the Sabzevar post-ophiolitic high silica adakitic rocks
Petrology and geochemistry of the Sabzevar post-ophiolitic high silica adakitic rocks

Habibollah Ghasemi; Khadijeh Jamshidi; Mahmoud Sadeghian

Volume 5, Issue 17 , April 2014, Pages 51-68

Abstract
  Some high silica adakitic domes with rhyolite, dacite, trachy-dacite, trachy-andesite and andesite compositions belonging to upper Eocene-Pliocene, trending W-NW, intruded in to the ...  Read More
Petrography and petrogenesis of Hasht-kuh Khezrabad of Yazd skarns
Petrography and petrogenesis of Hasht-kuh Khezrabad of Yazd skarns

Hossein Mehdizadeh Shahri; Javad Ghanei Ardakanei; Ali Darvishzadeh; Mohammad Ali Mackizadeh

Volume 5, Issue 17 , April 2014, Pages 69-82

Abstract
  The Khezr-Abad granitoid intrusive body is located in the north-west of Yazd province within Urumia-Dokhtar magmatic arc. The intrusion of this body into the Cretaceous carbonate rocks ...  Read More
Zircon U-Pb dating and geochemistry of Sarkhar and Bermani granitic rocks, East of Sangan iron mine, Khaf
Zircon U-Pb dating and geochemistry of Sarkhar and Bermani granitic rocks, East of Sangan iron mine, Khaf

Azadeh Malekzadeh Shafaroudi; Mohammad Hassan Karimpour; Seyed Ahmad Mazaheri; Abbas Golmohammadi

Volume 5, Issue 17 , April 2014, Pages 83-102

Abstract
  The Sarkhar and Bermani granitic rocks is located 300 km southeast of Mashhad, east of Sangan Mine, and northeastern Iran. Granitoid rock intruded older rocks such as crystalline limestone ...  Read More
Origin and tectonic setting of granitic rocks and dolerite dikes in the Nasrand pluton, southeast of Ardestan
Origin and tectonic setting of granitic rocks and dolerite dikes in the Nasrand pluton, southeast of Ardestan

Fatemeh Sarjoughian; Zahra Hamzei; Ali Kananian; Jamshid Ahmadian

Volume 5, Issue 17 , April 2014, Pages 103-118

Abstract
  The Nasrand pluton of Oligo-Miocene age, which is located approximately 40 km south-east of Ardestan, intruded into the Eocene volcanic rocks of the Urumieh-Dokhtar magmatic belt. This ...  Read More
Petrology of the Molataleb village granitoid (North of Aligudarz), NW of Isfahan, low temperature peraluminous I-type
Petrology of the Molataleb village granitoid (North of Aligudarz), NW of Isfahan, low temperature peraluminous I-type

Mahin Mansouri Esfahani; Mahmoud Khalili

Volume 5, Issue 17 , April 2014, Pages 119-136

Abstract
  The Molataleb granitoid lies in the Sanandaj-Sirjan Zone and composed of granodiorites, tonalites and minor diorites which intruded into the Jurassic (Lias-Dogger) shales and slates. ...  Read More
The major, minor and rare earth elements (REE)‍ variations in hydrothermal alteration zones in the volcanic rocks of the west of Naein ophiolite (Central Iran)
The major, minor and rare earth elements (REE)‍ variations in hydrothermal alteration zones in the volcanic rocks of the west of Naein ophiolite (Central Iran)

Neda Tavakoli; Elaheh Namnabat; Moussa Kalimi Noghreyan; Mohammad Ali Mackizadeh

Volume 5, Issue 17 , April 2014, Pages 137-150

Abstract
  The study area is located 39 km northwest of Naein and is a part of the Urumieh- Dokhtar volcano plutonic arc. The volcanic and pyroclastic rocks have been altered by hydrothermal fluids. ...  Read More