Muñoz, MercedesSagredo, J.Rincón Calero, P. J.Vegas, Ramón2015-09-022015-09-021996http://hdl.handle.net/10272/11083The 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 metamorphismspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Ductile-brittle shear-zoneMagmatic emplacementPluton of PájaraFuerteventuraCanary Islandsjournal articleopen access