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)
Aquifer geometry of Sahneh-Bisetun plain based onmorphotectonic and active faulting, Kermanshah province, Iran

Sh Chizari; H Nazari; A.R Karimi Bavandpur; M Fotovat; M Malek Mahmudi

Volume 26, Issue 102 , March 2017, , Pages 197-206

https://doi.org/10.22071/gsj.2017.44149

Abstract
  The NW-SE trendingSahneh-Bisetun Plain is located in the northeast of the Kermanshah province, and is extendedmore or less sub-parallel with the Zagros structural zone. The proximity of this plain with the Main Recent Fault (MRF) makes its study more important. In this study, in addition to the identification ...  Read More

Considering Factors Affecting High Arsenic Concentration in Groundwater Resources of Tabriz Plain Aquifers

A Asghari Moghaddam; R Barzegar

Volume 24, Issue 94 , March 2015, , Pages 177-190

https://doi.org/10.22071/gsj.2015.43280

Abstract
  The Tabriz plain with an area of more than 700 km2 is extended from the eastern limit of Tabriz city to the salt flats of UrmiaLake. There are two types of aquifers in this plain with different quality of groundwater. The unconfined aquifer, which is extended all over the plain, in recharge areas near ...  Read More

Studying Yazd Subsidence Using InSAR and Precise Leveling

M. Amighpey; S. Arabi; A. Talebi

Volume 20, Issue 77 , January 2010, , Pages 157-164

https://doi.org/10.22071/gsj.2010.55368

Abstract
  Blemish of subsidence and land ruptures such as destroying aquifer systems, damaging structures and disordering water main, are usually irreparable and expensive. One of the regions with a high rate subsidence in Iran is the Yazd-Ardakan plain that subsides with a maximum rate of 12 cm per year based ...  Read More