Emplazamiento en una zona de cizalla dúctil - frágil transtensiva para el Plutón de Pájara, Fuerteventura, Islas Canarias

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dc.contributor.authorMuñoz, Mercedes
dc.contributor.authorSagredo, J.
dc.contributor.authorRincón Calero, P. J.
dc.contributor.authorVegas, Ramón
dc.date.accessioned2015-09-02T09:13:47Z
dc.date.available2015-09-02T09:13:47Z
dc.date.issued1996
dc.description.abstractThe mésostructures within the host-rocks as well as the internal deformation ofthé Pájara Pluton in Fuerteventura, allow the definition of a N 5-15 E directed ductile-brittle transtensive shear-zone, that conditioned the emplacement of the intrusive core represented by this ptutonic body. We ha ve indirectly estimated an age of 22-21 Aia for this shear-zone, which is considered as coeval to the thermal metamorphismen_US
dc.identifier.urihttp://hdl.handle.net/10272/11083
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.otherDuctile-brittle shear-zoneen_US
dc.subject.otherMagmatic emplacementen_US
dc.subject.otherPluton of Pájaraen_US
dc.subject.otherFuerteventuraen_US
dc.subject.otherCanary Islandsen_US
dc.titleEmplazamiento en una zona de cizalla dúctil - frágil transtensiva para el Plutón de Pájara, Fuerteventura, Islas Canariasen_US
dc.titleEmplacement within a transtensive ductíle-bríttle shearzone for the pluton of Pájara, Fuerteventura, Canary Islandseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 21 (1996)