Geochemistry and source of tourmaline from the Soheyle-Pakuh granitoid body (North of Nain)
Geochemistry and source of tourmaline from the Soheyle-Pakuh granitoid body (North of Nain)

Mahin Mansouri Esfahani; Mohammad ‎ Bakhshi

Volume 9, Issue 2 , September 2018, , Pages 123-138

https://doi.org/10.22108/ijp.2017.104442.1032

Abstract
  The Oligocene Soheyle Pakuh granitoid body is located in the Urumieh- Dokhtar zone, which composed predominately of granodiorite, diorite and granite with mafic, aplite dikes and iron-tourmaline ...  Read More
Determination of P-T and tectonic setting of 
Ghaleh Yaghmesh plutonic complex (west of Yazd province)
 by using of mineral chemistry
Determination of P-T and tectonic setting of Ghaleh Yaghmesh plutonic complex (west of Yazd province) by using of mineral chemistry

Bahareh Fazeli; Mahmoud Khalili; Mahin Mansouri Esfahani

Volume 8, Issue 31 , December 2017, , Pages 43-66

https://doi.org/10.22108/ijp.2017.81993.0

Abstract
  The Ghaleh Yaghmesh plutonic massif is located the westernmost part of Yazd province and in the central part of the Urumieh – Dokhtar magmatic arc (UDMA). This massif with quartzdiorite, ...  Read More
Investigation of the geochemical and mineralogical characteristics of the dikes associated with copper mineralization at the southeastern Ardestan (NE Isfahan)
Investigation of the geochemical and mineralogical characteristics of the dikes associated with copper mineralization at the southeastern Ardestan (NE Isfahan)

Maryam Salehi; Zahra Alaminia; Mahin Mansouri Esfahani

Volume 8, Issue 30 , September 2017, , Pages 81-98

https://doi.org/10.22108/ijp.2017.81992

Abstract
  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. ...  Read More
The study of P-T formation of Kolah Ghazi granitoid based on mineralogical relationships (southeast of Isfahan)
The study of P-T formation of Kolah Ghazi granitoid based on mineralogical relationships (southeast of Isfahan)

Mahin Mansouri Esfahani; Mahmoud Khalili; Afsaneh Safari Mirghaleh; Khadijeh Khalili; Seyed Hassan Tabatabaei

Volume 6, Issue 24 , January 2016, , Pages 171-196

Abstract
  The Kolah Ghazi granitoid body is located in the south-southeast of Isfahan and lies in the Sanandaj-Sirjan zone. The pluton is predominately composed of monzogranite, granodiorite ...  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
Applicatiom of mineralography and fluid inclusion data to determine the formation conditions of porphyry copper deposit, NE Arak
Applicatiom of mineralography and fluid inclusion data to determine the formation conditions of porphyry copper deposit, NE Arak

Farimah Ayati; Houshang Asadi Harouni; Hashem Bagheri; Mahin Mansouri Esfahani

Volume 3, Issue 12 , March 2013, , Pages 15-32

Abstract
  The Dalli area located northeast of Arak and lies in the Urumieh-Dokhtar magmatic belt. The mineralized area is hosted by volcanic-subvolcanic bodies comprising of diorite-quartz diorite ...  Read More