Megacity of Tehran with a population of more than 8 million is located in a very active region, both in terms of tectonic and seismicity. Due to socio-economic and political importance of Tehran, in 1994 IIEES has initiated a comprehensive geotechnical hazard study in Tehran. The geotechnical microzonation part of the program was composed of two parts: site effect and liquefaction potential microzonation. Site effect microzonation was started for south of Tehran using one dimensional site response analysis and microtremor measurement. The results of these studies were compiled and presented in three microzonation maps for south of Tehran including: natural site period map, dynamic site period map and the PGA distribution map. Based on the p...
This paper presents an overview of the principles and practices of seismic microzonation with some c...
The purpose of this study is to develop a geotechnical microzonation model regarding the suitability...
An intense earthquake (MW = 6.4) occurred in western Iran, about 225 km west of Tehran at 7:28 local...
Azerbaijan is the site of convergent plate collisions along the Alpine-Himalayan active mountain bel...
The main purpose of this research is to show the current active faults and active tectonic of the ar...
Tehran has situated over several active faults such as Mosha, North Tehran, North Ray and South Ray ...
Mashhad city has a substantial risk of earthquakes due to the potential of the underlying soft soils...
Tehran, the capital city of Iran with a population of over 12 million, is one of the largest urban c...
Duzce in Turkey was severely damaged during the November 12th, 1999 earthquake (Mw 7.2). The paper p...
Considering the increasing population growth and the rapid growth of urbanization and pollution in t...
Various procedures were developed to evaluate liquefaction susceptibility of soil layers for impleme...
International audienceThis paper is concerned with the microseismicity and seismotectonics of the ea...
Tehran is placed in a high seismic risk zone with specific natural hazards. The resources to deal ef...
In this paper the site specific spectra for a region of the Zagros Mountains containing 5 cities in ...
Land subsidence is a worldwide phenomenon, where there is a sudden sinking or gradual downward settl...
This paper presents an overview of the principles and practices of seismic microzonation with some c...
The purpose of this study is to develop a geotechnical microzonation model regarding the suitability...
An intense earthquake (MW = 6.4) occurred in western Iran, about 225 km west of Tehran at 7:28 local...
Azerbaijan is the site of convergent plate collisions along the Alpine-Himalayan active mountain bel...
The main purpose of this research is to show the current active faults and active tectonic of the ar...
Tehran has situated over several active faults such as Mosha, North Tehran, North Ray and South Ray ...
Mashhad city has a substantial risk of earthquakes due to the potential of the underlying soft soils...
Tehran, the capital city of Iran with a population of over 12 million, is one of the largest urban c...
Duzce in Turkey was severely damaged during the November 12th, 1999 earthquake (Mw 7.2). The paper p...
Considering the increasing population growth and the rapid growth of urbanization and pollution in t...
Various procedures were developed to evaluate liquefaction susceptibility of soil layers for impleme...
International audienceThis paper is concerned with the microseismicity and seismotectonics of the ea...
Tehran is placed in a high seismic risk zone with specific natural hazards. The resources to deal ef...
In this paper the site specific spectra for a region of the Zagros Mountains containing 5 cities in ...
Land subsidence is a worldwide phenomenon, where there is a sudden sinking or gradual downward settl...
This paper presents an overview of the principles and practices of seismic microzonation with some c...
The purpose of this study is to develop a geotechnical microzonation model regarding the suitability...
An intense earthquake (MW = 6.4) occurred in western Iran, about 225 km west of Tehran at 7:28 local...