International audienceThe city of Eski?ehir in inner-western Turkey has experienced a destructive earthquake with Ms=6.4 in 1956 in addition to many events with magnitudes greater than 5. It is located in a wide basin having young sedimentary units and thick alluvium soils which also include liquefiable sand materials. There is also an active fault passing beneath the city center and the groundwater level is very close to the ground surface. Approximately 600 thousand people are living in the province of Eski?ehir. Therefore, the city and its vicinity have a high risk, when earthquake hazard is considered. This paper summarizes the probabilistic seismic hazard analysis (PSHA) which was performed for the province of Eski?ehir and introduces...
Stochastic methods are utilized for the assessment of seismic hazard for the Eskisehir region. A com...
This study is presented as a contribution to earthquake disaster mitigation studies for selected cit...
Due to the high complexity in the mechanism of earthquakes occurrence, it is not possible to predict...
International audienceThe city of Eski?ehir in inner-western Turkey has experienced a destructive ea...
The city of Eskişehir in inner-western Turkey has experienced a destructive earthquake with <I>...
Abstract: A probabilistic approach is applied to assess the seismic hazard in Turkey. This methodolo...
The capital and the second largest city of Turkey, Ankara, is generally considered to be safe in ter...
Using 4.0 and greater magnitude earthquakes which occurred between 1 January 1900 and 31 December 20...
While there has been significant research on probabilistic seismic hazard analysis (PSHA) using seve...
While there has been significant research on probabilistic seismic hazard analysis (PSHA) using seve...
WOS: 000438615600007The seismic zoning map of Turkey that is used in connection with the national se...
Makassar is one of Indonesian big cities with rapid growth rate, but not totally safe from earthquak...
Seismic hazard analysis of the earthquake-prone Eastern Anatolian Region (Turkey) has become more im...
The purpose of this study is to develop probabilistic hazard maps for Eskisehir including ءPeak Grou...
Nearly 108-km lengths of Mersin shores are composed of natural beaches. The region is located betwee...
Stochastic methods are utilized for the assessment of seismic hazard for the Eskisehir region. A com...
This study is presented as a contribution to earthquake disaster mitigation studies for selected cit...
Due to the high complexity in the mechanism of earthquakes occurrence, it is not possible to predict...
International audienceThe city of Eski?ehir in inner-western Turkey has experienced a destructive ea...
The city of Eskişehir in inner-western Turkey has experienced a destructive earthquake with <I>...
Abstract: A probabilistic approach is applied to assess the seismic hazard in Turkey. This methodolo...
The capital and the second largest city of Turkey, Ankara, is generally considered to be safe in ter...
Using 4.0 and greater magnitude earthquakes which occurred between 1 January 1900 and 31 December 20...
While there has been significant research on probabilistic seismic hazard analysis (PSHA) using seve...
While there has been significant research on probabilistic seismic hazard analysis (PSHA) using seve...
WOS: 000438615600007The seismic zoning map of Turkey that is used in connection with the national se...
Makassar is one of Indonesian big cities with rapid growth rate, but not totally safe from earthquak...
Seismic hazard analysis of the earthquake-prone Eastern Anatolian Region (Turkey) has become more im...
The purpose of this study is to develop probabilistic hazard maps for Eskisehir including ءPeak Grou...
Nearly 108-km lengths of Mersin shores are composed of natural beaches. The region is located betwee...
Stochastic methods are utilized for the assessment of seismic hazard for the Eskisehir region. A com...
This study is presented as a contribution to earthquake disaster mitigation studies for selected cit...
Due to the high complexity in the mechanism of earthquakes occurrence, it is not possible to predict...