Volume 32 (2022)
Volume 31 (2021)
Volume 30 (2020)
Volume 29 (2020)
Volume 28 (2019)
Volume 27 (2018)
Volume 26 (2017)
Volume 25 (2016)
Volume 24 (2015)
Volume 23 (2014)
Volume 22 (2013)
Volume 21 (2012)
Volume 20 (2011)
Volume 19 (2010)
Volume 18 (2009)
Volume 17 (2008)
Volume 16 (2007)
1. U-Pb Zircon Dating of Kuh-e Dom Intrusion, its Dikes and Enclaves

F Sarjoughian; A Kananian; A Esna-Ashari; J Ahmadian

Volume 24, Issue 95 , June 2015, , Pages 145-154


  The Kuh-e Dom intrusion with calc-alkaline nature, in the northeast of Ardestan is located in the central part of the Urumieh-Dokhtar Magmatic Arc and includes the felsic and intermediate-mafic units. The felsic unit consists of monzogranite, granodiorite, quartz monzonite and quartz monzodiorite, whereas ...  Read More

2. Compositional Zoning in Feldspars of the Kuh-e Dom Intrusive Rocks

F Sarjoughian; A Kananian; J Ahmadian

Volume 24, Issue 93 , December 2014, , Pages 133-146


  The alkali feldspars and plagioclases in the Kuh-e Dom intrusive rocks show compositionally and microtexturally zoning structure. The feldspar crystals in the various lithologies such as granite- granodiorite samples, diorite- gabbro samples and relatively high frequency microgranular mafic enclaves ...  Read More

3. Source and Tectonic Setting of Zarjebostan (NE of Qazvin) Paleogene Volcanic Rocks using REE and HFSE Elements

K. Kalantari; A. Kananian; A. Asiabanha; M. Eliassi

Volume 17, Issue 68 , February 2008, , Pages 140-149


      Paleogene basic to intermediate lava flows of Central Alborz, in the northeast of Qazvin city (Zarjebostan), include trachy-andesite, basaltic trachy-andesite and basaltic andesite. These volcanic rocks are high-K calc-alkaline rocks. Based on the high LILE/HFSE and LREE/HREE ratios ...  Read More

4. Petrology and Geochemistry of Qareaghaj Mafic – Ultramafic Intrusion, NW of Urmia

M. Mirmohammadi; A. Kananian

Volume 18, Issue 69 , February 2008, , Pages 177-191


        Qareaghaj mafic-ultramafic intrusion (QMUI) is located in northwest Iran, 36 km NW from Urmia city. The QUMI is composed mainly of non-mineralized mafic and Fe-Ti-P-rich ultramafic rocks (FTP). The mafic rocks, mainly coarse-grained gabbro, microgabbro, metagabbro and ortho-amphibolite, ...  Read More

5. Petrology and Tectonic Setting of Lakhshak Granodiorite, NW of Zahedan, Iran

A. Kananian; M. Rezaei-Kahkhaei; D. Esmaeili

Volume 17, Issue 65 , March 2007, , Pages 126-143


       The Lakhshak granitoid pluton which is located at 10 km northwest of Zahedan, has intruded into the Eocene flysch sediments with an elliptical shape and NW-SE direction. This pluton after emplacement has been cut by numerous dykes with NE-SW trend. These dykes comprised about ...  Read More