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 fault is located in seismic zone of Komes historical earthquake with Ms=7.9 (Ambraseys & Melville, 1982). Many people (more than 45000) were killed in Damghan city in Komes historical earthquake. In this paper, 4-5 paleo events along the Astaneh fault are presented through paleoseismological investigation
The occurrence of large to major earthquakes in Stable Continental Regions (SCR) is a rare phenomeno...
In this paper we present the results of preliminary geomorphic and trenching investigations along th...
The East Anatolian Fault Zone (EAFZ) is among the most important active continental transform fault ...
The 856 A.D. Qumis earthquake (M7.9) is the most destructive earthquake to have occurred in Iran, ki...
International audienceThe 856 A.D. Qumis earthquake (M7.9) is the most destructive earthquake to hav...
The North Tehran Fault is located at the southernmost piedmont of Central Alborz, north of Iran. It ...
International audienceThe North Tehran Fault (NTF) is located at the southernmost piedmont of Centra...
The ∼55 km-long Firouzkuh fault is located in the Central Alborz Mountains of Iran. It is a left-lat...
International audienceThe ∼55 km-long Firouzkuh fault is located in the Central Alborz Mountains of ...
International audienceThe Taleghan fault (TF) is a major active fault of the Central Alborz mountain...
The North Tabriz Fault is a major seismogenic fault in NW Iran. The last damaging earthquakes on thi...
International audiencePaleoseismology is a relatively young method of earthquake studies at the inte...
is the easternmost part that ruptured during the 17 August 1999 İzmit earthquake (Mw 7.4). It has a ...
This study contributes paleoseismological data on the recent history of surface-rupturing earthquake...
West Central Iran comprises numerous Quaternary faults. Having either strike-slip or thrust mechanis...
The occurrence of large to major earthquakes in Stable Continental Regions (SCR) is a rare phenomeno...
In this paper we present the results of preliminary geomorphic and trenching investigations along th...
The East Anatolian Fault Zone (EAFZ) is among the most important active continental transform fault ...
The 856 A.D. Qumis earthquake (M7.9) is the most destructive earthquake to have occurred in Iran, ki...
International audienceThe 856 A.D. Qumis earthquake (M7.9) is the most destructive earthquake to hav...
The North Tehran Fault is located at the southernmost piedmont of Central Alborz, north of Iran. It ...
International audienceThe North Tehran Fault (NTF) is located at the southernmost piedmont of Centra...
The ∼55 km-long Firouzkuh fault is located in the Central Alborz Mountains of Iran. It is a left-lat...
International audienceThe ∼55 km-long Firouzkuh fault is located in the Central Alborz Mountains of ...
International audienceThe Taleghan fault (TF) is a major active fault of the Central Alborz mountain...
The North Tabriz Fault is a major seismogenic fault in NW Iran. The last damaging earthquakes on thi...
International audiencePaleoseismology is a relatively young method of earthquake studies at the inte...
is the easternmost part that ruptured during the 17 August 1999 İzmit earthquake (Mw 7.4). It has a ...
This study contributes paleoseismological data on the recent history of surface-rupturing earthquake...
West Central Iran comprises numerous Quaternary faults. Having either strike-slip or thrust mechanis...
The occurrence of large to major earthquakes in Stable Continental Regions (SCR) is a rare phenomeno...
In this paper we present the results of preliminary geomorphic and trenching investigations along th...
The East Anatolian Fault Zone (EAFZ) is among the most important active continental transform fault ...