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)
Archaeoseismological investigation along the Khazar fault system, based on the Paleoseismology (Gohar Tappeh protohistory Site, Behshahr- Mazandaran)

Z. Bakhtiarizadeh; H. Nazari; M. A. Shokri; A. Mahfroozi; A. Kaveh-firooz

Volume 28, Issue 110 , December 2018, , Pages 209-220

https://doi.org/10.22071/gsj.2019.84444

Abstract
  Archaeologists believe that men who lived in Archaeological sites of Mazandaran such as Komishan cave, Hutu and Kamarband, After leaving the cave were gradually formed the Gohar tappeh. Over time, people living with the loss of previous places were higher places. In Neolithic village has been form of ...  Read More

Paleoseismologic Activity and Subsidence Rate on Tehran Alluvium Deposits in Chitgar Section; using Paleoseismological Data

A. Kaveh Firouz; H. Nazari; M. Arian; A. Shafei; T. Majidi; M. Shokri

Volume 21, Issue 84 , December 2012, , Pages 169-178

https://doi.org/10.22071/gsj.2012.53978

Abstract
  The North Tehran Fault with a length of about 110 km in North of Tehran and soutern of central Alborz with W-E trend (N25˚E) and dipping (30˚NE) is located in western of Mosha Fault.The branch of Chitgar such as Milad and Vardavard Fault in the form of propagation fault is increased toward south. Previous ...  Read More

First Records of 1384 AD Shahr-e-Rey’s Historical Earthquake on Pishva Fault based on Paleoseismology Researches, South East of Tehran

T. Majidi Niri; H. Nazari; M. Ghorashi; M. Talebian; A. Kaveh Firooz

Volume 21, Issue 81 , December 2011, , Pages 169-178

https://doi.org/10.22071/gsj.2011.54381

Abstract
  Pishva fault with about 35km length is located between Alborz and Central Iran structural zones in southeast of Varamin. General trend of the fault is NW-SE (N38W, 33NE) which has reverse mechanism accompanied by sinistral component. Achieved Morphotectonic studies along the Pishva fault reveal its activity.  ...  Read More