Resumen de Emplazamiento en una zona de cizalla dúctil - frágil transtensiva para el Plutón de Pájara, Fuerteventura, Islas Canarias.
Mercedes Muñoz, J. Sagredo, Pedro José Rincón Calero, Ramón Vegas Martínez
The mesostructures within the host-rocks as well as the internal deformation of the 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 plutonic body. We have indirectly estimaled an age of 22-21 Ma for this shear-zone, which is considered as coeval to the thermal metamorphism.
