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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>2018-01-15T18:37:29Z</responseDate> <request identifier=oai:HAL:insu-00769762v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:insu-00769762v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:phys</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CEA</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:UNIV-BREST</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>openaire</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>The Gibraltar subduction: A decade of new geophysical data</title> <creator>Gutscher, Marc-André, </creator> <creator>Dominguez, Stephane</creator> <creator>Westbrook, Graham K.</creator> <creator>Le Roy, Pascal, </creator> <creator>Rosas, F.</creator> <creator>Duarte, J.C.</creator> <creator>Terrinha, P.</creator> <creator>Miranda, J.M.</creator> <creator>Graindorge, David</creator> <creator>Gailler, A.</creator> <creator>Sallarès, V.</creator> <creator>Bartolome, R.</creator> <contributor>Domaines Océaniques (LDO) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université de Brest (UBO) - Observatoire des Sciences de l'Univers - Institut d'écologie et environnement - 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>University Birmingham ; University of Birmingham [Birmingham]</contributor> <contributor>Geology Department ; University of Lisbon</contributor> <contributor>School of Geosciences ; Monash University [Clayton]</contributor> <contributor>IDL, Universidade de Lisboa, Lisbon ; Université du Québec</contributor> <contributor>FFCUL/CGUL Centro de Geofisica ; Universidade de Libsoa</contributor> <contributor>Commissariat à l'Energie Atomique ; Commissariat à l'énergie atomique et aux énergies alternatives (CEA)</contributor> <contributor>Unitat de Tecnologia Marina ; Centre Mediterrani d'Investigacions Marines I ambientals</contributor> <description>International audience</description> <source>ISSN: 0040-1951</source> <source>EISSN: 1879-3266</source> <source>Tectonophysics</source> <publisher>Elsevier</publisher> <identifier>insu-00769762</identifier> <identifier>https://hal-insu.archives-ouvertes.fr/insu-00769762</identifier> <source>https://hal-insu.archives-ouvertes.fr/insu-00769762</source> <source>Tectonophysics, Elsevier, 2012, 574-575, pp.72-91. 〈10.1016/j.tecto.2012.08.038〉</source> <identifier>DOI : 10.1016/j.tecto.2012.08.038</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2012.08.038</relation> <language>en</language> <subject lang=en>Iberia</subject> <subject lang=en>Roll-back subduction</subject> <subject lang=en>Tethys oceanic lithosphere</subject> <subject lang=en>Accretionary wedge</subject> <subject lang=en>Active deformation</subject> <subject lang=en>Earthquakes</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>The Gibraltar arc, spans a complex portion of the Africa-Eurasia plate boundary marked by slow oblique convergence and intermediate and deep focus seismicity. The seemingly contradictory observations of a young extensional marine basin surrounded by an arcuate fold-and-thrust belt, have led to competing geodynamic models (delamination and subduction). Geophysical data acquired in the past decade provide a test for these models and support a narrow east-dipping, subduction zone. Seismic refraction studies indicate oceanic crust below the western Gulf of Cadiz. Tomography of the upper mantle reveals a steep, east-dipping high P-wave velocity body, beneath Gibraltar. The anisotropic mantle fabric from SKS splitting shows arc-parallel "fast directions", consistent with toroidal flow around a narrow, westward retreating subducting slab. The accompanying WSW advance of the Rif-Betic mountain belt has constructed a thick pile of deformed sediments, an accretionary wedge, characterized by west-vergent thrust anticlines. Bathymetric swath‐mapping images an asymmetric embayment at the deformation front where a 2 km high basement ridge has collided. Subduction has slowed significantly since 5 Ma, but deformation of recent sediments and abundant mud volcanoes suggest ongoing activity in the accretionary wedge. Three possible origins for this deformation are discussed; gravitational spreading, overall NW-SE convergence between Africa and Iberia and finally a WSW tectonic push from slow, but ongoing roll-back subduction. In the absence of arc volcanism and shallow dipping thrust type earthquakes, evidence in favor of present-day subduction can only be indirect and remains the object of debate. Continued activity of the subduction offers a possible explanation for great (M > 8.5) earthquakes known to affect the area, like the famous 1755 Great Lisbon earthquake. Recent GPS studies show SW motion of stations in N Morocco at velocities of 3-6 mm/yr indicating the presence of an independent block, a "Rif-Betic-Alboran" microplate, situated between Iberia and Africa.</description> <date>2012-10-29</date> <contributor>European Project : 34220, NEAREST</contributor> <relation>info:eu-repo/grantAgreement//34220/EU/INTEGRATED OBSERVATIONS FROM NEAR SHORE SOURCES OF TSUNAMIS: TOWARDS AN EARLY WARNING SYSTEM/NEAREST</relation> </dc> </metadata> </record> </GetRecord> </OAI-PMH>