untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T18:41:10Z</responseDate>
<request identifier=oai:HAL:hal-00670999v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:hal-00670999v1</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>Crustal resistivity structure of the southwestern transect of the Rif Cordillera (Morocco)</title>
<creator>Anahnah, Farida</creator>
<creator>Galindo-Zaldivar, Jesus</creator>
<creator>Chalouan, Ahmed</creator>
<creator>Pous, Jaume</creator>
<creator>Ruano, Patricia</creator>
<creator>Pedrera, Antonio</creator>
<creator>RUIZ-CONSTAN, Ana</creator>
<creator>Ahmamou, M'Fedal</creator>
<creator>Benmakhlouf, Mohamed</creator>
<creator>Ibarra, Pedro</creator>
<creator>Asensio, Eva</creator>
<contributor>Departamento de Geodinámica, Universidad de Granada ; Université du Québec</contributor>
<contributor>Département de Géologie ; Université du Québec</contributor>
<contributor>Departament de Geodinàmica i Geofísica [Barcelona] ; Universitat de Barcelona (UB)</contributor>
<contributor>Instituto Geológico y Minero de España (IGME)</contributor>
<contributor>Manteau et Interfaces ; 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) - 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 de Géologie, Université Abdelmalek Esaadi, Tetuán ; Université du Québec</contributor>
<contributor>Instituto Geológico y Minero de España [Granada] ; Instituto Geológico y Minero de España (IGME)</contributor>
<description>International audience</description>
<source>ISSN: 1525-2027</source>
<source>EISSN: 1525-2027</source>
<source>Geochemistry, Geophysics, Geosystems</source>
<publisher>AGU and the Geochemical Society</publisher>
<identifier>hal-00670999</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00670999</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00670999</source>
<source>Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2011, 12, pp.Q12016. 〈10.1029/2011GC003783〉</source>
<identifier>DOI : 10.1029/2011GC003783</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2011GC003783</relation>
<language>en</language>
<subject lang=en>Gibraltar Arc</subject>
<subject lang=en>broadband magnetotelluric</subject>
<subject lang=en>crustal detachments</subject>
<subject lang=en>deep structure</subject>
<subject lang=en>exotic blocks</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>A NE-SW magnetotelluric 110 km-long profile including 18 sites was acquired across the western Rif Cordillera along the Eurasian-African plate boundary, allowing to constrain its poorly known deep structure. It extends from the Internal Zones, close to the Alboran coast, crossing the External Zones and up to the Gharb foreland basin. The periods recorded range from 0.001 s to 1000 s. The combination of magnetotelluric data with available geological data provides new insight regarding the relationship between deep and shallow crustal structures of the Rif Cordillera. Analyses of structural dimensionality suggest a preferential NW-SE direction, and a 2D joint inversion was performed. A 3D inversion extending the 2D model along the strike confirmed the reliability of this approach. The magnetotelluric model shows a heterogeneous upper crust in agreement with the geological structures observed at surface. The Internal Zones correspond to resistive (metamorphic rocks) and conductive (peridotites) bodies, while the External Zones and the foreland basin are characterized by large conductive bodies of variable thickness. A crustal detachment level separating shallow geological units from a probable variscan basement was inferred. At depth, the most relevant feature consists of large resistive bodies with a shallow irregular top, located below the frontal part of the Rif. The outcrops of exotic metapelitic, granitic and gneissic blocks in the frontal part of the Cordillera suggest that these large resistive bodies may correspond to a gneissic or granitic basement surrounded by metapelitic rocks. Late contractive thrust and diapiric processes were responsible for their uplift and shallow emplacement. The Rif constitutes an active southwestward vergent orogenic wedge, oblique to the present-day NW-SE convergent Eurasian-African plate boundary.</description>
<date>2011</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
