Contribution of ultramafic rocks in central Sanandaj-Sirjan zone to the characterizing of physio-chemical condition during initiation of subduction
Contribution of ultramafic rocks in central Sanandaj-Sirjan zone to the characterizing of physio-chemical condition during initiation of subduction

Amir Esna-Ashari; Fatemeh Sarjoughian

Volume 8, Issue 32 , March 2018, , Pages 45-66

https://doi.org/10.22108/ijp.2017.100430.0

Abstract
  In the central part of the Sanandaj-Sirjan zone, there is an ultramafic rock exposure (hornblendite and pyroxenite) adjacent to Molataleb felsic complex completely located between Azna ...  Read More
The composition of the major minerals in the Nasrand intrusive rocks and its dikes
The composition of the major minerals in the Nasrand intrusive rocks and its dikes

Ali Kananian; Jamshid Ahmadian; Fatemeh Sarjoughian

Volume 6, Issue 21 , April 2015, , Pages 35-54

Abstract
  The Nasrand intrusion, in the central part of Uromieh-Dokhtar magmatic belt is mainly composed of granite and granodiorite. The intrusive rocks are hosted by various dikes trending ...  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
Application of pyroxene chemistry for evaluation of temperature and pressure in the Kuh-e Dom intrusion
Application of pyroxene chemistry for evaluation of temperature and pressure in the Kuh-e Dom intrusion

Fatemeh Sarjoughian; Ali Kananian; Jamshid Ahmadian

Volume 3, Issue 11 , December 2012, , Pages 97-110

Abstract
  The Late Eocene Kuh-e-Dom intrusion located in the central part of Urumieh-Dokhtar magmatic belt, NE of Ardestan. The intrusion consists of gabbroic to granitic rocks, intruded by several ...  Read More