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<datestamp>2018-01-11</datestamp>
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<title lang=en>Using luminescence dating of coarse matrix material to estimate the slip rate of the Astaneh fault, Iran</title>
<creator>Rizza, Magali</creator>
<creator>Mahan, S.</creator>
<creator>Ritz, Jean-François</creator>
<creator>Nazari, H.</creator>
<creator>Hollingsworth, J.</creator>
<creator>Salamati, Reza</creator>
<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>US Geological Survey [Denver] ; United States Geological Survey [Reston] (USGS)</contributor>
<contributor>Research Institute for Earth Sciences ; Geological Survey of Iran</contributor>
<contributor>Division of Geological and Planetary Sciences [Pasadena] ; California Institute of Technology (CALTECH)</contributor>
<source>ISSN: 1871-1014</source>
<source>Quaternary Geochronology</source>
<publisher>Elsevier</publisher>
<identifier>hal-00617777</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00617777</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00617777</source>
<source>Quaternary Geochronology, Elsevier, 2011, 6 (3-4), pp.390-406. 〈10.1016/j.quageo.2011.03.001〉</source>
<identifier>DOI : 10.1016/j.quageo.2011.03.001</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quageo.2011.03.001</relation>
<language>en</language>
<subject lang=en>Luminescence dating</subject>
<subject lang=en>Tectonics</subject>
<subject lang=en>Alluvial fans</subject>
<subject lang=en>Geomorphology</subject>
<subject lang=en>Faulting</subject>
<subject lang=en>Iran</subject>
<subject lang=en>Alborz</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>In this paper, we present optically and infrared stimulated luminescence (OSL and IRSL) ages for four samples from alluvial fan surfaces in the Astaneh Valley. This valley is located in the north-east part of the Alborz range in Iran. Our morphologic interpretations recognize at least three generations of fans in the study area, all of which have been displaced along the left-lateral strike-slip Astaneh fault. Because of the dry, loose, and sometimes complex juxtaposition of the target sediments, we collected the samples in total darkness beneath dark plastic layers placed atop the pit openings. Luminescence ages of the fans are similar to 55 ka, similar to 32 ka and similar to 16 ka. These ages are concurrent with periods of loess deposition and wet climatic conditions previously recorded in the Arabia-Iranian region. They allow estimation of a horizontal slip rate of similar to 2 mm/yr along the Astaneh fault, which is consistent with additional slip rates determined for the Holocene period along faults further west of the Astaneh fault.</description>
<date>2011</date>
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