La serie volcánica submarina del Complejo Basal de Fuerteventura: crecimiento submarino y emersión de la Isla

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dc.contributor.authorGutiérrez, M.
dc.contributor.authorCasillas Fernández, R.
dc.contributor.authorBalogh, K.
dc.contributor.authorAhijado, A.
dc.contributor.authorCastillo, Carolina
dc.date.accessioned2014-11-18T13:57:30Z
dc.date.available2014-11-18T13:57:30Z
dc.date.issued2002
dc.description.abstractThree lithological units have been distinguished in the volcanic succession of the Basal Complex of Fuerteventura Island, from bottom to top: the Submarine Volcanic Croup, the Transitional Volcanic Croup and the Subaerial Volcanic Croup. These units record the submarine growth and the emersion of the Island. During these stages the volcanism is represented by an ultraalkaline and a strongly alkaline igneous series. The igneous activity was due to the presence of an anomalous zone in the sublithospheric mantle and influenced by the Cenozoic tectonic evolution of the northwestern part of the African plateen_US
dc.identifier.urihttp://hdl.handle.net/10272/9344
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherBasal Complexen_US
dc.subject.otherSubmarine growthen_US
dc.subject.otherEmersionen_US
dc.subject.otherFuerteventuraen_US
dc.subject.otherCanary Islandsen_US
dc.titleLa serie volcánica submarina del Complejo Basal de Fuerteventura: crecimiento submarino y emersión de la Islaen_US
dc.titleThe submarine volcanic succesion of the Basal Complex of Fuerteventura: submarine growth and emersion of the Islandeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 32, (2002)