Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/47899
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dc.contributor.authorVizcaíno, A.-
dc.contributor.authorGràcia, Enric-
dc.contributor.authorPallàs i Serra, Raimon-
dc.contributor.authorTerrinha, P.-
dc.contributor.authorEscutia, C.-
dc.contributor.authorDañobeitia, Juan José-
dc.contributor.authorJacobs, Carla-
dc.contributor.authorHITS Cruise Party (incl. G. Lastras)-
dc.date.accessioned2013-11-19T18:32:07Z-
dc.date.available2013-11-19T18:32:07Z-
dc.date.issued2004-
dc.identifier.issn1576-5172-
dc.identifier.urihttp://hdl.handle.net/2445/47899-
dc.description.abstractThe Southwest Iberian Margin is caracterized by an intense and diffuse seismic activity due to the convergence between Eurasian and African plates...-
dc.format.extent4 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherSociedad Geológica de España-
dc.relation.ispartofGeo-Temas, 2004, vol. 6, num. 5, p. 215-218-
dc.rights(c) Sociedad Geológica de España, 2004-
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)-
dc.subject.classificationValls submarines-
dc.subject.classificationEuropa-
dc.subject.classificationFalles (Geologia)-
dc.subject.otherSubmarine valleys-
dc.subject.otherEurope-
dc.subject.otherFaults (Geology)-
dc.titleEstudio de alta resolución de las fallas activas y procesos sedimentarios asociados al Cañón de São Vicente, margen Sudoeste de Iberia-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec533846-
dc.date.updated2013-11-19T18:32:07Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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