Please use this identifier to cite or link to this item: http://dspace.mediu.edu.my:8181/xmlui/handle/10261/4491
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dc.creatorBorque Arancón, María Jesús-
dc.creatorGalindo-Zaldívar, Jesús-
dc.creatorGil, Alejandro J.-
dc.creatorJabaloy, Antonio-
dc.creatorLacy Pérez de los Cobos, M.ª Clara de-
dc.creatorLópez-Garrido, A. C.-
dc.creatorRodríguez Caderot, Gracia-
dc.creatorRuíz Armenteros, Antonio-
dc.creatorSanz de Galdeano, Carlos-
dc.date2008-05-23T10:25:55Z-
dc.date2008-05-23T10:25:55Z-
dc.date2005-
dc.date.accessioned2017-01-31T01:26:57Z-
dc.date.available2017-01-31T01:26:57Z-
dc.identifierFísica de la Tierra 2005, 17, 23-31-
dc.identifier0214-4557 (Print)-
dc.identifier1988-2440 (Online)-
dc.identifierhttp://hdl.handle.net/10261/4491-
dc.identifier.urihttp://dspace.mediu.edu.my:8181/xmlui/handle/10261/4491-
dc.descriptionThe NW-SE to NNW-SSE convergence between the African and Eurasian plates in the western Mediterranean has developed the recent relief of the Betic-Rif Cordilleras. The central part of the Internal Zones of the Betic Cordilleras is deformed by large open folds and faults, mainly with normal character. The Zafarraya fault, located to the N of the Sierra Tejeda antiform, was active during the 1884 Andalusia earthquake of 6.7 estimated magnitude. In the framework of an interdisciplinary research project, a non-permanent GPS-network has been established at Zafarraya Fault and Sierra Tejeda antiform to monitor deformations related to these active tectonic structures.-
dc.descriptionPeer reviewed-
dc.format3798409 bytes-
dc.formatapplication/pdf-
dc.languageeng-
dc.publisherUniversidad Complutense de Madrid-
dc.rightsopenAccess-
dc.subjectActive Tectonics-
dc.subjectGPS Network-
dc.subjectZafarraya Fault-
dc.subjectSierra Tejeda Antiform-
dc.subjectBetic Cordillera-
dc.titleEstablishment of a non-permanent GPS network to monitor deformations in Zafarraya Fault and Sierra Tejeda Antiform (Spain)-
dc.typeArtículo-
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