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)
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

https://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

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

https://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

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

https://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