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
Petrography and application of mineral chemistry and thermobarometry of amphibolites in Jandaq metamorphic complex: Evidence of paleo-tectonic events in Central Iran

Arefeh Heidarianmanesh; Seyed Mohsen Tabatabaimanesh; Narges Shirdashtzadeh

Volume 32, Issue 4 , December 2022, , Pages 119-142

https://doi.org/10.22071/gsj.2022.329201.1981

Abstract
  Based on field observation and petrographic evidence, by progress in metamorphic degrees, a wide variety of metabasites have formed following the metamorphism at amphibolite facies (metamorphism M1) in the east of Jandaq. Thermobarometry of plagioclase- amphibole pairs indicate temperature ranges were ...  Read More

Petrology
Mineralogy and determination of thermodynamic conditions at Javinan Skarn, South of Kashan

S. M. Tabatabaei Manesh; M. A. Mackizadeh; saeideh ranjbar; R. Gholinezhad

Volume 28, Issue 109 , September 2018, , Pages 327-338

https://doi.org/10.22071/gsj.2017.72014.1008

Abstract
  Javinan skarn is located at 115 km north west  of  Isfahan (40 km south of Kashan and east of Ghohrud), is included  in Central Iran structural zone and spread in contact with Ghohrud granitoid (Middle Miocene age) with shale, sandstone and limestone succession of the Jurassic age known ...  Read More

Mineral chemistry and petrogenesis of East Nabar skarn, Southwest of Kashan

S. M. Tabatabaei Manesh; F. Javadi; F. S Zohouri2

Volume 27, Issue 107 , June 2018, , Pages 253-264

https://doi.org/10.22071/gsj.2018.63836

Abstract
  The Nabar skarn is located about 35 km southwest of Kashan and within the Urumieh- Dokhtar magmatic belt  and is formed along the contact between limestone of Qom formation with a probably middle to upper Miocene intermediate and basic intrusion body. The main minerals forming this skarn are garnet, ...  Read More

Mineralogy of Garnet in Khuni Skarn, Northeast of Anarak, Isfahan Province: Evidences for a Hydrothermal System Evolution

S Ranjbar; S.M Tabatabaei manesh; M.A Mackizadeh

Volume 25, Issue 97 , December 2016, , Pages 173-182

https://doi.org/10.22071/gsj.2015.41423

Abstract
  The Khuni skarn has been developed in the contact between small tongues of the Late Eocene-Oligocene I-type Kal-e kafi granitoidic intrusive body and the Precambrian Lakh marble-dolomite unit, Located 220 km northeast of Esfahan in the Central Iran structural zone. Skarnification could be divided into ...  Read More

Geotectonic Investigation of Early Paleozoic Magmatism inUrumieh- Dokhtar Zone (South of Kashan)

S. M. Tabatabaeimanesh; H. Safaei; A. S. Mirlohi

Volume 20, Issue 78 , December 2011, , Pages 47-52

https://doi.org/10.22071/gsj.2010.54588

Abstract
  In south of Kashan, early Paleozoic volcanic rocks are a part of Ghohrudmountains. In Iran structural- sedimentary division, these volcanic rocks located inUrumieh- Dokhtar zone. These volcanic rocks are basic to semibasic and mostly involved basalt. Geochemical investigations of these rocks show the ...  Read More