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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>2018-01-15T15:43:05Z</responseDate> <request identifier=oai:HAL:insu-00304360v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:insu-00304360v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:phys</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-BREST</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> <setSpec>collection:LGO</setSpec> <setSpec>collection:CMM</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Propagators and ridge jumps in a back-arc basin, the West Philippine Basin</title> <creator>Deschamps, Anne</creator> <creator>Shinjo, Ryuichi</creator> <creator>Matsumoto, Takeshi</creator> <creator>Lee, Chao-Shing</creator> <creator>E. Lallemand, Serge</creator> <creator>Wu, Shiguo</creator> <creator>Party Of Kr03-04 And Kr04-14 Cruises, Scientific</creator> <contributor>Domaines Océaniques (LDO) ; Centre National de la Recherche Scientifique (CNRS) - Institut d'écologie et environnement - Observatoire des Sciences de l'Univers - Université de Brest (UBO) - Institut national des sciences de l'Univers (INSU - CNRS)</contributor> <contributor>Department of Physics and Earth Sciences ; University of the Ryukyus [Okinawa]</contributor> <contributor>Institute of Applied Geophysics ; National Taiwan Ocean University (NTOU)</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>Institute of Oceanology [CAS] (IOCAS) ; Chinese Academy of Sciences [Changchun Branch] (CAS)</contributor> <description>International audience</description> <source>ISSN: 0954-4879</source> <source>EISSN: 1365-3121</source> <source>Terra Nova</source> <publisher>Wiley-Blackwell</publisher> <identifier>insu-00304360</identifier> <identifier>https://hal-insu.archives-ouvertes.fr/insu-00304360</identifier> <source>https://hal-insu.archives-ouvertes.fr/insu-00304360</source> <source>Terra Nova, Wiley-Blackwell, 2008, 20 (4), pp.327-332. 〈10.1111/j.1365-3121.2008.00824.x〉</source> <identifier>DOI : 10.1111/j.1365-3121.2008.00824.x</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-3121.2008.00824.x</relation> <language>en</language> <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 explore the tectono-magmatic processes in the western West Philippine Basin, Philippine Sea Plate, using bathymetric data acquired in 2003 and 2004. The northwestern part of the basin formed through a series of northwestward propagating rifts. We identify at least five sequences of propagating rifts, probably triggered by mantle flow away from the mantle thermal anomaly that is responsible for the origin of the Benham and Urdenata plateaus. Gravitational forces caused by along-axis topographic gradient and a ∼30° ridge reorientation appear to also be driving the rift propagations. The along-axis mantle flow appears to be reduced and deflected along the Luzon-Okinawa fracture zone, because the spreading system remained stable west of this major fault zone. North-east of the Benham plateau, a left-lateral fracture zone has turned into a NE–SW-trending spreading axis. As a result, a microplate developed at the triple junction.</description> <date>2008-07-21</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>