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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T15:41:45Z</responseDate> <request identifier=oai:HAL:hal-00407957v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00407957v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Luminescence dating of a gigantic palaeolandslide in the Gobi-Altay mountains, Mongolia</title> <creator>Balescu, S.</creator> <creator>Ritz, Jean-Francois</creator> <creator>Lamothe, M.</creator> <creator>Auclair, M.</creator> <creator>Todbileg, M.</creator> <contributor>Préhistoire et environnements quaternaires de l'Europe du nord-ouest (PEQENO) ; Université de Lille, Sciences et Technologies - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>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)</contributor> <contributor>Département des Sciences de la Terre et de l'Atmosphère, Université du Québec, Montréal ; Université du Québec</contributor> <contributor>School of Geology, Mongolian University of Science and Technology, Ulaanbaatar ; Université du Québec</contributor> <source>ISSN: 1871-1014</source> <source>Quaternary Geochronology</source> <publisher>Elsevier</publisher> <identifier>hal-00407957</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00407957</identifier> <source>https://hal.archives-ouvertes.fr/hal-00407957</source> <source>Quaternary Geochronology, Elsevier, 2007, 2 (1-4), pp.290-295. 〈10.1016/j.quageo.2006.05.026〉</source> <identifier>DOI : 10.1016/j.quageo.2006.05.026</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quageo.2006.05.026</relation> <language>en</language> <subject lang=it>Luminescence dating</subject> <subject lang=it>Palaecolandslide</subject> <subject lang=it>Mongolia</subject> <subject lang=it>Pleistocene</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 an attempt to date a palaeolandslide that took place along the Baga Bogd Massif, in Mongolia, the infrared stimulated luminescence (IRSL) method has been applied to lacustrine silty sediments directly overlying the landslide mass. The IRSL age estimates obtained on alkali feldspar grains (>40 μm) and polymineral fine grains (4–11 μm) provide a minimum age for the landslide event. The IRSL ages on alkali feldspars corrected for long-term fading using the protocol of Mejdahl (1988, 1989) suggest that the palaeolandslide occurred at the beginning of the Last Interglacial. These are in good agreement with the ;10;Be cosmogenic dates obtained on faulted and abandoned alluvial fans in the Gobi-Altay mountains. This study demonstrates for the first time that the IRSL dating method can successfully be applied for establishing landslide chronologies.</description> <date>2007</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>