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)
Petrology
1. Geochemistry and tectonic setting of Tertiary lavas in Abbas Abad area(Northeast of Sarbisheh), Southern Khorasan

Marziyeh Abazari; Seyyed Saeid Mohammadi; Malihe Nakhaei

Volume 29, Issue 114 , December 2019, , Pages 41-50

http://dx.doi.org/10.22071/gsj.2018.133273.1478

Abstract
  Abbas Abad area is located in the northeast of Sarbisheh, in the northern part of Sistan suture zone and southern Khorasan province. In this area, Tertiary volcanic rocks with the composition of intermediate to acid, including basaltic andesite, andesite, and dacite are exposed. Constructive minerals ...  Read More

Petrology
2. Geochemistry, tectonic environment and origin of Oligo-Miocene lavas in Zoolesk area, northeast of Sarbisheh (Southern Khorasan)

Maryam Kouchi; Malihe Nakhaei

Volume 28, Issue 110 , December 2018, , Pages 255-266

http://dx.doi.org/10.22071/gsj.2018.94302.1214

Abstract
  In northeast of Sarbisheh city, southern Khorasan, outcrops of lava rocks are exist that from view of geological subdivisions, located in eastern part of Lut block. Lithologic composition of studied collections consist of andesite (pyroxene andesite, andesite, trachy andesite), dacite and rhyolite. The ...  Read More

3. Petrology, geochemistry and geochronology of Nodoushan intrusive complex, West of Yazd

B. Shahsavari Alavijeh; N. Rashidnejad Omran; J. Ghalamghash

Volume 27, Issue 105 , December 2017, , Pages 215-232

http://dx.doi.org/10.22071/gsj.2017.53952

Abstract
  The Nodoushan intrusive complex is a part of Cenozoic plutonism, which located in the central part of the Urumieh–Dokhtar Magmatic Belt (UDMB). This complex consists of four main intrusives, including diorite, granite-granodiorite, diorite porphyry and granodiorite. Mafic microgranular enclaves ...  Read More

4. Geochemistry, petrogenesis and tectonic setting of the Sarcheshmeh Eocene mafic lava flows, Southwest of Rafsanjan

S.Z Hosseini

Volume 25, Issue 100 , September 2016, , Pages 209-220

http://dx.doi.org/10.22071/gsj.2016.42264

Abstract
  The Eocene mafic lava flows of Sarcheshmehare cropped out in the southwest of Rafsanjan area at the central part of the Urmia – Dokhtar magmatic belt. The rocks are basalt, basaltic andesite and andesite in composition and consist of clinopyroxene + plagioclase ± olivine ± hornblende phenocrysts. ...  Read More

5. Petrology of Intrusive Bodyes in Jebale-Barez Granitoid Complex (South East Jiroft)

J Rasouli; M Ghorbani; V Ahadnejad

Volume 24, Issue 96 , September 2015, , Pages 3-16

http://dx.doi.org/10.22071/gsj.2015.41665

Abstract
  Jebale-Barez granitoid complex is composed of intrusive bodyes included Mijan, Dareh hamzeh, Kerver and Hishin and is located In the southeastern province of Kerman on the lengths of the 57◦ 45 ' east to   58◦ 00' and Northern latitudes 28◦ 30' to 29◦ 00'.The petrologic composition ...  Read More

6. Vein-type and Stratabound W (Cu-Au) Mineralization in Iran

S Ghaderi; E Rastad; N Rashidnejad-Omran; M Mohajjel

Volume 24, Issue 94 , March 2015, , Pages 305-314

http://dx.doi.org/10.22071/gsj.2015.42949

Abstract
  Tungsten (Cu-Au-Zn) deposits and occurrences in Iran can be divided into two separate categories based on their genesis, tectonic setting, mineral paragenesis and related processes inherent in their formation. The first category contains deposits, which are located in metamorphosed Late Triassic-Middle ...  Read More

7. 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

http://dx.doi.org/10.22071/gsj.2009.57853

Abstract
      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