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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>2018-01-15T15:41:30Z</responseDate> <request identifier=oai:HAL:hal-00411313v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00411313v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:phys</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-CERGY</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:UPMC</setSpec> <setSpec>collection:ISTEP</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:UPMC_POLE_3</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Source model for the Mw 6.1, 31 March 2006, Chalan-Chulan earthquake (Iran) from InSAR</title> <creator>Peyret, Michel</creator> <creator>Rolandone, Frédérique</creator> <creator>Dominguez, Stephane</creator> <creator>Djamour, Y.</creator> <creator>Meyer, Bertrand</creator> <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>Laboratoire de tectonique (LT) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Cergy Pontoise - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>National Cartographic Center [Iran] (NCC)</contributor> <source>ISSN: 0954-4879</source> <source>EISSN: 1365-3121</source> <source>Terra Nova</source> <publisher>Wiley-Blackwell</publisher> <identifier>hal-00411313</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00411313</identifier> <source>https://hal.archives-ouvertes.fr/hal-00411313</source> <source>Terra Nova, Wiley-Blackwell, 2008, 20 (2), pp.126-133. 〈10.1111/j.1365-3121.2008.00797.x〉</source> <identifier>DOI : 10.1111/j.1365-3121.2008.00797.x</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-3121.2008.00797.x</relation> <language>en</language> <subject lang=en>Main recent fault</subject> <subject lang=en>neighborhood algorithm</subject> <subject lang=en>geophysical inversion</subject> <subject lang=en>radar interferometry</subject> <subject lang=en>Zagros mountains</subject> <subject lang=en>GPS measurements</subject> <subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject> <subject>[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]</subject> <subject>[SDE.MCG] Environmental Sciences/Global Changes</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>We use InSAR to measure deformation and kinematics of the Mw = 4.9 Borujerd (2005/05/03) and Mw = 6.1 Chalan-Chulan (2006/03/31) earthquakes that occurred in the Zagros fold-and-thrust belt. The focal mechanism of the 2006 event is consistent with right lateral strike-slip motion and the event ruptured the Dorud-Borujerd segment of the Main Recent Fault. An Envisat interferogram spanning the 2006 event shows peak ground deformation of 9 cm in the satellite line-of-sight along a 10 km long fault portion. The interferogram spanning the 2005 earthquake is rather related to atmospheric artefact than to ground deformation. Dislocation models of the 2006 Chalan-Chulan event indicate dextral slip amounting to a maximum of 90 cm at a depth of 4 km. The predicted vertical displacements are in good agreement with differential levelling data. The 2006 event filled only a small part of the seismic gap located between large M = 7 events that occurred in 1909 and 1957.</description> <date>2008</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>