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
Genesis of the Miandasht manto-type copper deposit, East of Mayamey: based on geological, mineralogical and geochemical evidences

Fardin mousivand; Fatemeh Esmaeili; Mahmoud Sadeghian; Seyed Mehran Heidari

Articles in Press, Corrected Proof, Available Online from 26 February 2022

http://dx.doi.org/10.22071/gsj.2022.293355.1919

Abstract
  Miandasht copper deposit is located in 24km north west of Abbasabad of Shahrood, and in the Cenozoic volcanic belt of north of Central Iran. Host sequence has Eocene age and include submarine flows (andesite and basalt), pyroclastic (tuff breccia and agglomerate) and sedimentary complex (Nomullitic limestone, ...  Read More

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

http://dx.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

Sedimentology
Ore facies, ore horizons and genesis of the Gol-e-Zard sedeimentary-exhalative (SEDEX) zinc-lead, Lorestan province

hajar ghafleh maramazi; Fardin mousivand; alireza zarasvandi

Volume 30, Issue 118 , January 2021, , Pages 153-164

http://dx.doi.org/10.22071/gsj.2020.151062.1545

Abstract
  The Gol-e-Zard zinc-lead deposit is located in the Malayer-Isfahan belt of Sanandaj-Sirjan zone in northeast of Aligudarz, Lorestan province. Mineralization occurred as two different ore horizon within metamorphosed Jurassic shale and sandstone. Generally, two ore facieses were distinguished in the deposit: ...  Read More

Economic Geology
Nohkuhi volcanogenic massive sulfide deposit: a sample of Bathurst- type mineralization in northwest of Kerman

Amir Pakizeh; Fardin mousivand; Abdorrahman Rajabi; Sajjad Maghfouri

Volume 29, Issue 115 , June 2020, , Pages 111-122

http://dx.doi.org/10.22071/gsj.2019.117154.1397

Abstract
  The Nohkuhi copper deposit located at 40 Km Northwest of Kerman, occurred in the Central Iran structural zone (Bafq- Posht-e- Badam block), within Late Precambrian-Early Cambrian volcano-sedimentary sequences. Host sequence of mineralization consists of dominantly black shale, sandstone and dacitic lava ...  Read More

Economic Geology
Geology, geochemistry and genesis of the Darreh Amrood Pb (Ag) deposit in the Urumieh-Dokhtar magmatic arc, south of Ghohrood

Fardin mousivand; Fayeq Hashemi; Mehdi Rezaei-Kahkhaei; Amir Pakizeh

Volume 29, Issue 114 , December 2019, , Pages 259-268

http://dx.doi.org/10.22071/gsj.2018.122431.1438

Abstract
  The Darreh Amrood Pb (Ag) deposit is located in south of Ghohrood, in the Urumieh-Dokhtar magmatic arc (UDMA). Host rockes to the deposit are Middle to Late Eocene grey-green siliceous tuff and crystal lithic tuff. Geometry of orebodies is stratabound, irregular, and semiconcordant to discordant to layering ...  Read More

Ore facies, alteration zoning and physico-chemical conditions of formation of the Bavanat (Jian) Besshi-type Cu-Zn-Ag volcanogenic massive sulfide deposit, Fars province

F Mousivand; E Rastad; M.H Emami; J Peter; M Solomon

Volume 25, Issue 99 , June 2016, , Pages 61-74

http://dx.doi.org/10.22071/gsj.2016.40771

Abstract
  The Bavanat (Jian) pelitic-mafic- / Besshi-type Cu-Zn-Ag volcanogenic massive sulfide deposit locates in the Bavanat area, South Sanandaj-Sirjan zone. Mineralization occurs as two stratigraphic ore horizons discontinuously within the Surian metamorphosed volcano-sedimentary complex through more than ...  Read More

Nudeh Volcanogenic Massive Sulfide (VMS) Deposit, A Besshi- Type VMS Deposit, Southwest Sabzevar

S Maghfouri; E Rastad; F Mousivand; Y Lin

Volume 24, Issue 94 , March 2015, , Pages 73-86

http://dx.doi.org/10.22071/gsj.2015.42744

Abstract
  Copper mineralization in Nudeh Cu deposit and Frezy, Garab, Kalateh lala (Nieran) and Chun occurrences, located in southwest of Sabzevar hosted by a Upper Cretaceous volcano-sedimentary sequence formed in a rift environment. The main is host rock of the Nudeh Cu sulfide deposit includes alkali olivine ...  Read More

Formation of Various Types of Volcanogenic Massive Sulfide (VMS) Deposits and Its Relationship With Tectono-Magmatic Evolution in the Sanandaj-Sirjan Zone

F Mousivand; E Rastad; M.H Emami; J.M Peter

Volume 23, Issue 90 , March 2014, , Pages 11-21

http://dx.doi.org/10.22071/gsj.2014.43901

Abstract
  Various types of volcanogenic massive sulfide (VMS) deposits occurred within the northern and southern parts of the Sanandaj-Sirjan zone (SSZ). The most important VMS deposits of the south SSZ includes the Bavanat Cu-Zn-Ag (pelitic mafic- or Besshi-type), Sargaz Cu-Zn (bimodal mafic- or Noranda-type), ...  Read More

Structure in the Chah Gaz Zn-Pb-Cu Massive Sulfide Deposit,South of Shahr-e -Babak

K. Orang; Mohammad Mohajjel; F. Mousivand; E. Rastad

Volume 22, Issue 86 , December 2012, , Pages 193-202

http://dx.doi.org/10.22071/gsj.2012.54085

Abstract
  The Chah Gaz Zn-Pb-Cu volcanogenic massive sulfide (VMS) deposit is a polydeformed, polymetamorphosed ore body in southern part of the Sanandaj-Sirjan zone. The ore bodies are comprised predominantly of stratiform, tabular and lenticular massive sulfide lenses and are elongated in 0600-0700 orientation. ...  Read More

Bathurst-type Zn-Pb-Cu Volcanogenic Massive Sulfide Mineralization in the Chahgaz Area, South of Shahre Babak, South Sanandaj-Sirjan Zone

F. Mousivand; E. Rastad; M. H. Emami; J. M. Peter; M. Solomon

Volume 21, Issue 82 , December 2011, , Pages 151-164

http://dx.doi.org/10.22071/gsj.2011.54451

Abstract
  Zn-Pb-Cu mineralization in the Chahgaz area, located 60 km south of Shahre Babak, occurs within a Middle Jurassic metamorphosed bimodal volcano-sedimentary sequence in the South Sanandaj-Sirjan zone. Mineralization occurs associated with exhalites within units 1and 2 of the host sequence as numerous ...  Read More