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)
Economic Geology
Ore facies, geochemistry and genesis of Kuhe Rig Fe-Sr-(Mn) deposit, South of Shahroud

Mona Mahdevari; Fardin mousivand; Mahmoud Sadeghian; Mehdi Movahednia

Volume 31, Issue 2 , September 2021, , Pages 79-90

https://doi.org/10.22071/gsj.2020.189496.1666

Abstract
  Kuhe Rig iron- strontium-(manganese) deposit is located in south of Shahrood, in the northern part of the central Iran zone. Mineralization occurred in the Eocene volcano-sedimentary sequence dominated by andesite basalt, basalt and crystal lithic tuffs. Geometry of main ore body is lense-shaped which ...  Read More

Economic Geology
Study of geology, mineralogy and geochemistry of the Robaei iron deposit, South Damghan

faraj fardoost; Akbar Abdollahi Hydarbaghi; Solmaz Baluchi

Volume 29, Issue 115 , June 2020, , Pages 61-74

https://doi.org/10.22071/gsj.2019.109101.1338

Abstract
  The Robaei Iron deposit is located in 96km south of Damghan. Host rocks of deposit are Late Cretaceous limestones (part I) and Eocene volcano- sedimentary rocks including sandy tuff (part II.( The alterations include chloritization, epidotization, argillation, silicification, carbonatization and hematitization. ...  Read More

Economic Geology
Thermobarometric Properties of Epigenitic Mineralization Based on Fluid Inclusion Data in Dehkoyeh Salt Dome, Lar, Fars Province

Mohammad Jabarian; mehrdad karimi; Mohammad Lotfi; kamal noori khankahdani

Volume 29, Issue 115 , June 2020, , Pages 289-300

https://doi.org/10.22071/gsj.2018.93957.1210

Abstract
  Dehkooye salt dome is located 30 km northeast of Lar in Fars province, Iran. The salt dome occurred in Zagros folded zone where infracambrian thick evaporate strata (Hormoz series) intruded Cenozoic sedimentary rocks. Core of the dome mainly made up of salt and gypsum and overlain by marl, gypsum, limestone, ...  Read More

Mineralization, geochemistry, fluid inclusion and stable isotopes (O, S) studies in the Takht Fe-skarn deposit, NE Hamedan

S. N. Haghighi Bardineh; R. Zarei Sahamieh; H. Zamanian; A. Ahmadi Khalaji

Volume 27, Issue 107 , June 2018, , Pages 99-112

https://doi.org/10.22071/gsj.2018.63797

Abstract
  The Takht iron deposit is located 120 km northeast of the Hamedan City in the Urumieh-Dokhtar magmatic belt. The Miocene Takht granodiorite intruded into the Cretaceous carbonates and resulted in Fe-skarn formation. Epigenetic mineralization in the Takht Deposit occurred predominantly as vein and lenticular ...  Read More

Mineralization Stages and Iron Source of Bashkand Deposit Based on Mineralogy, Structure, Texture and Geochemical Evidence, Southwest of Soltanieh

S Shahbazi; M Ghaderi; N Rashidnejad-Omran

Volume 24, Issue 95 , June 2015, , Pages 355-372

https://doi.org/10.22071/gsj.2015.42471

Abstract
  The Bashkand iron deposit is located in 16 km southwest of Soltanieh, in Central Iran Structural Zone. The rock units in the area include alternations of metamorphosed sedimentary rocks of the Kahar Formation, Khorramdarreh granite and an andesitic dike. The major alteration types are argillic, potassic, ...  Read More

Stages and Mineralization Conditions of Dardvey Iron Skarn Based on Mineralogy and Fluid Inclusion Evidences, Sangan Area (Khorasan Razavi)

E. Tale Fazel; B. Mehrabi; A. Khakzad; R. Kianpour

Volume 21, Issue 82 , December 2011, , Pages 139-150

https://doi.org/10.22071/gsj.2011.54450

Abstract
  Sangan iron ore deposit is located in 308 km southeast of Mashhad and eastern structural zone of Iran. Due to the high grade, low P-content and high reserve, Sangan is regarded as one of the major iron ore deposits in Iran. The important anomalies in Sangan consist of east, central and west anomalies ...  Read More

Mineralogy, Geochemistry and Origin of Iron Deposits in North of Semnan

A. R. Ghiasvand; M. Ghaderi; N. Rashidnejad-Omran

Volume 18, Issue 72 , January 2009, , Pages 33-44

https://doi.org/10.22071/gsj.2010.57133

Abstract
  The iron deposits in north of Semnan are located in the south of Central Alborz structural zone. Stratigraphically, the area consists of Paleozoic to Quaternary rock series exposures. The area has been affected by Semnan, Darjazin, Attari and Diktash faults. An intermediate to acidic granitoid body of ...  Read More