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<identifier>oai:HAL:hal-00854396v1</identifier>
<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Preliminary results of paleoseismological trenching along the Astaneh fault</title>
<creator>Shokri, M.</creator>
<creator>Ghorashi, M.</creator>
<creator>Nazari, Amid</creator>
<creator>Salamati, Reza</creator>
<creator>Talebian, Morteza</creator>
<creator>Ritz, Jean-François</creator>
<creator>Mohammad Khani, H.</creator>
<creator>Shahpasand Zadeh, H.</creator>
<contributor>West Tehran Islamic Azad University [Tehran] (WTIAU)</contributor>
<contributor>Teacher Training University ; Teacher Training University - Université du Québec</contributor>
<contributor>Research Institute for Earth Sciences, Geological Survey of Iran, Tehran ; Université du Québec</contributor>
<contributor>Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>International Institute of Earthquake Engineering and Seismology, Tehran ; Université du Québec</contributor>
<source>Geosciences Scientific Quarterly Journal</source>
<identifier>hal-00854396</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00854396</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00854396</source>
<source>Geosciences Scientific Quarterly Journal, 2008, 18, pp.84-93</source>
<language>fa</language>
<subject lang=en>paleoseismology</subject>
<subject lang=en>Historical earthquake</subject>
<subject lang=en>Morphotectonics</subject>
<subject lang=en>Paleo-event</subject>
<subject lang=en>Damghan</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>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.</description>
<date>2008-01-01</date>
</dc>
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