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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>2018-01-15T15:41:35Z</responseDate> <request identifier=oai:HAL:hal-00411144v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00411144v1</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:SDE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</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>Present-day movements of tectonic blocks in the Betic-Rif Arc from GPS measurements 1999-2005</title> <creator>Tahayt, A.</creator> <creator>Mourabit, T.</creator> <creator>Rigo, A.</creator> <creator>Feigl, K. L.</creator> <creator>Fadil, A.</creator> <creator>Mcclusky, S.</creator> <creator>Reilinger, R.</creator> <creator>Serroukh, M.</creator> <creator>Ouazzani-Touhami, A.</creator> <creator>Ben Sari, D.</creator> <creator>Vernant, Philippe</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> <source>ISSN: 0010-7999</source> <source>EISSN: 1432-0967</source> <source>Contributions to Mineralogy and Petrology</source> <publisher>Springer Verlag</publisher> <identifier>hal-00411144</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00411144</identifier> <source>https://hal.archives-ouvertes.fr/hal-00411144</source> <source>Contributions to Mineralogy and Petrology, Springer Verlag, 2008, 340 (6), pp.400-413. 〈10.1016/j.crte.2008.02.003〉</source> <identifier>DOI : 10.1016/j.crte.2008.02.003</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2008.02.003</relation> <language>en</language> <subject lang=en>GPS</subject> <subject lang=en>seismotectonics</subject> <subject lang=en>Rif</subject> <subject lang=en>Alboran</subject> <subject lang=en>block</subject> <subject lang=en>present-day tectonics</subject> <subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</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>GPS velocities and seismicity across the Betic-Rif Arc structural domains (Morocco and Iberia) provide a basis to evaluate present-day seismotectonic processes between different deformation belts. The results show asymmetric movements in the complex Alboran system accommodating the convergence between the African (Nubian) and Eurasian plates. While the Betic Mountains are attached to Iberia, moving toward the southeast with respect to Africa, the Rif is divided into three blocks with distinct displacements relative to Nubia: (1) the Tangier block moving southeastward, (2) the Central Rif block moving SSW, and (3) the Oriental Rif block undergoing clockwise rotation. GPS-derived motions decrease in rate from the Rif nappes complex to the foreland.</description> <date>2008</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>