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)
Chronology of Last Earthquake on Firouzkuh Fault using by C14

Hamid Nazari; J-F Ritz; R Walker; R Salamati; A Ghasemi; A Shafei

Volume 19, Issue 76 , January 2010, , Pages 95-98

https://doi.org/10.22071/gsj.2010.55665

Abstract
  The Firouzkuh Fault in most of its extension is located at the southern side of Firouzkuh Valley in west of the Central Alborz.  It is a SW – NE prominent structure with a 70 km long on a sinistral –normal fault. It has been known as a south-dipping reverse fault.Paleoseismic analysis ...  Read More

Preliminary Results of Paleoseismologic Trenching along the Astaneh Fault

M. Shokri; M. Ghorashi; H. Nazari; R. Salamati; M. Talebian; J.-F. Ritz; H. Mohammad khani; M. Shahpasand zadeh

Volume 18, Issue 70 , February 2009, , Pages 84-93

https://doi.org/10.22071/gsj.2009.57378

Abstract
  The Astaneh fault with a length of more than 75 km is located in NW of Damghan. Morphotectonic investigation along the Astaneh fault and left - lateral displacement in quaternary deposits shows that, Astaneh is an active fault. It is necessary to recognize paleoseismicity of Astaneh fault because, this ...  Read More

Linear Structures in South of Tehran (Reys and Kahrizak "Faults"): Fault Scarps or Geomorphologic Phenomenon?!

H. Nazari; J-F. Ritz; R. Salamati; M. Ghorashi; A. Ghasemi; H. Habibi; F. Jamali; Sh. Javadipur

Volume 19, Issue 73 , January 2009, , Pages 109-114

https://doi.org/10.22071/gsj.2010.57206

Abstract
  Tehran and its surrounding region are within affecting zone of some active faults of North Tehran and Mosha in north-north east and Parchin and Pishva in south.  In addition, there are some other shorter faults and linear markers within the urban area of Tehran such as Niavaran, Mahmoudieh and Davoudieh ...  Read More

Kinematic and Geometry of the Taleghan Active Fault: On the Basis of Morphotectonics Studies, (Central Alborz, Iran)

H. Nazari; J-F. Ritz

Volume 18, Issue 71 , January 2009, , Pages 173-177

https://doi.org/10.22071/gsj.2010.57011

Abstract
  The Taleghan Fault is located at the southern side of Taleghan valley in Central Alborz, 50 km north west of the Tehran mega city. Usually described as a south-dipping reverse fault, it could be the source of some of the strongest historical earthquakes recorded in the Tehran region, notably the 958 ...  Read More

New Insight to Paleogeography and Structural Evolution of the Alborz in Tethyside

H. Nazari; J-F. Ritz; S. Oghbaee

Volume 16, Issue 64 , March 2007, , Pages 38-53

https://doi.org/10.22071/gsj.2008.58213

Abstract
  Development and evolution of Tethys basins during geological history from the Precambrian to Paleogene has been considered by many geoscientists.  The first sign of various basins propagation of Tethys which resulted in separation of supercontinents, ancient lands (such as Eurasia, Gondwana) and ...  Read More