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
Petrography and Geochemistry of tourmaline nodules from Aderba leucogranite (northeast of Golpaygan)
Petrography and Geochemistry of tourmaline nodules from Aderba leucogranite (northeast of Golpaygan)

Akramosadat Mirlohi; Mahmoud Khalili

Volume 7, Issue 27 , October 2016, , Pages 191-205

https://doi.org/10.22108/ijp.2016.21029

Abstract
  The Aderba leucogranite in the Golpayegan metamorphic core complex (GMC), a part of Sanandaj-Sirjan zone, host lentiform small (2*4 cm)(Type 1) and large (7*14 cm)(Type 2)tourmaline ...  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
Petrography and mineral chemistry of alteration zones in the Kahang porphyry Cu-Mo deposit (Northeast of Isfahan)
Petrography and mineral chemistry of alteration zones in the Kahang porphyry Cu-Mo deposit (Northeast of Isfahan)

Farimah Ayati; Hashem Bagheri; Hooshang Asadi Harooni; Mahmoud Khalili; Salimeh sadat Komeili

Volume 5, Issue 19 , December 2014, , Pages 1-20

Abstract
  The study area is located in the Uromieh-Dokhtar volcanic belt and composed of andesite-basalt, andesite, dacite and quartz-monzonite as volcanic and subvolcanic. The occurrence of ...  Read More
Volcanic and subvolcanic rocks dating in the north of Shahrekord by 40Ar/39Ar method, a new approach regarding the occurrence andduration of the Jurassic volcanism in the Sanandaj-Sirjan zone
Volcanic and subvolcanic rocks dating in the north of Shahrekord by 40Ar/39Ar method, a new approach regarding the occurrence andduration of the Jurassic volcanism in the Sanandaj-Sirjan zone

Sayed Naeim Emami; Mahmoud Khalili

Volume 5, Issue 18 , November 2014, , Pages 1-14

Abstract
  The volcano - sedimentary complex in the north of Shahrekord as a belt with NW-SW trendand 396 km2 area is parallel to the Zagros structural zone within the central part of the Sanandaj- ...  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
Sodic-calcic alteration in the host rocks of the Esfordi magnetite-apatite deposit
Sodic-calcic alteration in the host rocks of the Esfordi magnetite-apatite deposit

Sedigheh Taghipour; Ali Kananian; Mahmoud Khalili

Volume 4, Issue 13 , April 2013, , Pages 67-80

Abstract
  The host rocks of the Esfordi deposit consist of rhyolitic tuff lower Camrianand rhyolite along with dolomites of the Rizu series which are widely affected by sodic-calcic hydrothermal ...  Read More
Petrographic and mineral-chemistry of the magmatic-alteration zones South of Salafchegan
Petrographic and mineral-chemistry of the magmatic-alteration zones South of Salafchegan

Farimah Ayati; Moussa Kalimi Noghreyan; Mahmoud Khalili

Volume 2, Issue 8 , January 2012, , Pages 1-20

Abstract
  The study area which lies along the Uromieh-Dokhtar volcanic belt, comprises andesi-basalt, andesite, dacite, diorite and quartz-diorite with porphyry texture exposing as volcanic and ...  Read More
Petrographical and geochemical characteristics of enclaves in Astaneh area (Southwest of Arak)
Petrographical and geochemical characteristics of enclaves in Astaneh area (Southwest of Arak)

Zara Tahmasbi; Mahmoud Khalili; Ahmad Ahmadi Khalaji

Volume 2, Issue 6 , November 2011, , Pages 31-46

Abstract
  The Astaneh granodiorite intrusion, located in the southwest of Arak, is characterized by rounded and rarely ellipsoid microgranular enclaves ranging in composition from gabbro to diorite ...  Read More
Mineral chemistry of mantle peridotites from Loghar ophiolite (Southweast of Kabul - Afghanistan)
Mineral chemistry of mantle peridotites from Loghar ophiolite (Southweast of Kabul - Afghanistan)

Gholamhossein Nazari; Ghodrat Torabi; Mahmoud Khalili

Volume 2, Issue 5 , June 2011, , Pages 19-48

Abstract
  The Loghar ophiolite is located in ophiolitic belt of Kabul block (southeast of Afghanistan) and it is a part of Neotethyan ophiolites in Alpine - Himalayan orogenic system with Eocene ...  Read More
Petorgenesis of the granitoid body in the south of Shazand (South western Arak)
Petorgenesis of the granitoid body in the south of Shazand (South western Arak)

Zahra Tahmasbi; Mahmoud Khalili; Ahmad Ahmadi khalaji; Mohammad Ali Makki zadeh

Volume 1, Issue 1 , June 2010, , Pages 87-102

Abstract
  The Astaneh granitoid massif represents a small portion of Sanandaj – Sirjan zone and consists of tonalite, granodiorite, monzogranite and rhyodacite, being the granodiorites ...  Read More