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
Mineralogy, geochemistry, fluid inclusion study and genesis of Homeijan magnetite- apatite mineralization, SW Behabad, Yazd province

R. Amirkhani; M. Ebrahimi; M. A. A. Mokhtari; A. M. Azimzadeh

Volume 26, Issue 103 , June 2017, , Pages 83-100

https://doi.org/10.22071/gsj.2017.46732

Abstract
  The study area which is introduced as Homeijan magnetite- apatite mineralization in this paper, is a part of the Posht-e-Badam block in the Central Iranian Zone and is located at ~12Km southwest of Behabad. This area is composed of volcano-sedimentary rocks and acidic- basic intrusions of Precambrian ...  Read More

Petrology and geochemistry of Homijan granitoid and associated felsic rocks (SW Behabad, Central Iran)

F Mohamadi; M Ebrahimi; M.A.A Mokhtari

Volume 25, Issue 98 , March 2016, , Pages 223-236

https://doi.org/10.22071/gsj.2016.41219

Abstract
  The study area,~12 km to the southwest of the city Behabad, is a part of the Posht-e-Badam Block in Central Iran. Igneous rocks in the area occur as intrusive, sub-volcanic and volcanic bodies and exhibit a wide range of composition from felsic to mafic. The intrusive and sub- volcanic rocks include ...  Read More

Tectonic Activity Rate in Behabad Area According to Morphotectonic Indices, NE Yazd Province, Iran

M Sheban; F Ghaemy; A Abbasnejad; F Ghaemy

Volume 23, Issue 91 , June 2014, , Pages 141-152

https://doi.org/10.22071/gsj.2014.43802

Abstract
  Neotectonics that is a major factor of landform development in tectonically active regions has significantly affected fluvial systems and mountain-front landscapes in the Behabad area of the Central Iran Zone. To assess tectonic activities in the area, we analyzed geomorphic indices including the mountain-front ...  Read More