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)
Investigation on Stream Displacements Along Parts of the Doruneh Fault

H Amini; M Fattahi; M.R Ghassemi

Volume 23, Issue 92 , September 2014, , Pages 209-218

https://doi.org/10.22071/gsj.2014.43704

Abstract
  The Doruneh fault is the second longest fault systems in Iran. This fault is 700 km long and extended from the Afghanistan-Iran border to the central Iran desert. Despite of its length, and position in the convergence zone between the Arabian and Eurasian plates and its seismic potential, only one historical ...  Read More

Late Pliestocene-Holocene Paleoseismicity, Temporal Clustering, & Probabilities of Future Large (M>7) Earthquake on the Dehshir Fault, Central Iran

M Foroutan; H Nazari; B Meyer; M Sébrier; M Fattahi; K Le Dortz; M Ghorashi; Kh Hessami; M. R Ghassemi; M Talebian

Volume 23, Issue 90 , March 2014, , Pages 75-90

https://doi.org/10.22071/gsj.2014.43958

Abstract
  The Dehshir fault system (DFS) including six fault segments forms the western border of NS-striking active dextral strike-slip fault cutting the Sanandaj-Sirjan, Uromieh-Dokhtar magmatic arc, and Central Iran. This active fault system right-laterally offset Eocene volcanic rocks and Quaternary alluvial ...  Read More

Late Pleistocene-Holocene Right- Slip Rate of The Dehshir Fault, Central Iran Plateau

M Foroutan; H. Nazari; B. Meyer; M. Sébrier; M. Fattahi; K. Le Dortz; M. Ghorashi; Kh. Hessami; M. R. Ghassemi; M. Talebian

Volume 21, Issue 82 , December 2011, , Pages 195-206

https://doi.org/10.22071/gsj.2011.54458

Abstract
  The evaluation of  seismic potential along the Dehshir fault with 550-km  length (by count of northern and southern splays) is critical considering that more than 3.5 million people live in cities and towns located at vicinity of the fault. The Dehshir fault is considered as westernmost limit ...  Read More

An Investigation into the Activity of the Neyshabour Fault, Khorasane Province, Iran

M. Fattahi; S. Rostami Mehraban; M. Talebian; A. Bahroudi; J. Hollingsworth; R. Walker

Volume 20, Issue 79 , January 2011, , Pages 55-60

https://doi.org/10.22071/gsj.2018.55006

Abstract
  Neyshabour (approximately 200,000 pop.) lies on the southern margin of the Binalud mountains in NE Iran.  The city has been destroyed four times by major historical earthquakes (in 1209, 1270, 1389 and 1405 A.D.).Three large faults occur in the region.  The Binalud and North Neyshabur faults ...  Read More

Estimating Slip Rates of Faults around Bam and their Application in Evaluation of Earthquake Hazard

M. Talebian; S. H. Tabatabaei; M. Fattahi; M. Ghorashi; A. Beitollahi; A. Ghalandarzadeh; M.A. Riahi

Volume 19, Issue 74 , February 2010, , Pages 149-156

https://doi.org/10.22071/gsj.2010.57347

Abstract
  The Iranian plateau lies between the Arabian and Eurasian plates and accommodates approximately 22 mm/yr of N-S shortening.  About 9 mm/y of this shortening is taken up by folding and thrusting in the Zagros while the remaining 13 mm/yr is taken up in the Alborz and Kopeh-Dagh. The Central Iran ...  Read More

Detection of Recent Activity on Doruneh Fault Using Remote Sensing Data and Geological Information

H. Amini; M. Fattahi; M. R. Ghassemi

Volume 19, Issue 76 , January 2010, , Pages 57-62

https://doi.org/10.22071/gsj.2010.55646

Abstract
  Doruneh is an active left- lateral strike- slip fault in North-East Iran.  Surface trace of this fault is about 700 km long, and cuts across Quaternary and Tertiary deposits.  In some places along the fault, sediments of Paleogene.  Neogene, and alluvial fans of Quaternary age are displaced ...  Read More