Volume 34 (2024)
Volume 33 (2023)
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
Petrogenesis of granitoids from Dalfard area (Northwest of Jiroft): Evidence of Volcanic arc tectonic setting in Urumieh – Dokhtar magmatic belt

Zeinab Rahmanian; Gholam Reza Ghadami; Hamid Ahmadipour; Mohammad Poosti

Volume 33, Issue 1 , February 2023, , Pages 123-142

https://doi.org/10.22071/gsj.2022.349172.2010

Abstract
  Dalfard granitoids are located in the south-east of Kerman province and in the margins mainly include quartz diorite. Quartz diorites contain main minerals plagioclase, amphibole and biotite  and this work reveals that the rocks in this area are I type granitoides and they belong to calc-alkaline ...  Read More

Petrology
Geochemistry and origin of the ortho- amphibolites inTakhte-Soleyman (NE Takab)

Ziba Khodaean Chegeni; Nematollah Rashidnejad Omran; Ali Akbar Baharifar; Reza Nozaem; Carmela Vaccaro; José Francisco Santos

Volume 32, Issue 2 , July 2022, , Pages 133-148

https://doi.org/10.22071/gsj.2021.295726.1920

Abstract
  Takhte-Soleyman ortho-amphibolites as a part of Takab metamorphic complex are located in Northeast Takab. These rocks consist of amphibolite, Garnet-amphibolite, Kyanite-Garnet-amphibolite, Hornblendite and Epidote-amphibolite. Petrography and whole- rock geochemistry show that basalt, andesite and/or ...  Read More

Petrography, origin and magmatic evolution of Khunrang intrusive complex, northwest of Jiroft, Kerman

S Sedighian; S Dargahi; M Arvin

Volume 26, Issue 102 , March 2017, , Pages 207-220

https://doi.org/10.22071/gsj.2017.44150

Abstract
  Khunrang intrusive complex, as a one of the largest complexes in the southern part of the Sanandaj-Sirjan zone, is located at northwest of Jiroft, in Kerman province. The complex mainly consists of acidic-intermediate rocks such as diorite, quartzdiorite, tonalite, granodiorite, and granite with subordinate ...  Read More

Petrological, Geochemical and Tectonomagmatic Setting of Bouin- Miandasht Intrusion in Sanandaj- Sirjan Zone(SSZ) (West of Iran)

M. Sabeti; M. H. Emami; A. Saeedi; K. Ajdary; A. Minaee; A. R. Nadimi

Volume 21, Issue 84 , December 2012, , Pages 43-56

https://doi.org/10.22071/gsj.2012.53955

Abstract
  Bouin– Miandasht Intrusive body is located in South- West of Golpayegan quadrangle and Sanandaj- Sirjan Zone. This Intrusion is composed of a compositional range including: porphyroid granite (monzogranite- syenogranite), granodiorite and gabbro – diorite. Variation diagrams of major and ...  Read More

Geochemistry and Petrogenesis of the Orzuieh Volcanic Sequence (South of Iran)

I. Monsef; M. Rahgoshay; M. H. Emami

Volume 21, Issue 82 , December 2011, , Pages 65-76

https://doi.org/10.22071/gsj.2011.54442

Abstract
  The Late Jurassic to Early Cretaceous Orzuieh volcanic sequence is exposed in the southern part of the Sanandaj – Sirjan Zone. Major and trace element geochemistry shows magma evolution from the transitional to the calc-alkaline series. Clinopyroxene compositions are similar to their composition ...  Read More