Estudio comparativo de los cuerpos intrusivos básicos asociados a los materiales de edad triásica de los dominios Subbético y Nevado-Filábride del sector Centro-Oriental de las cordilleras béticas

Abstract

The basic intrusive bodies, from both Subbetic and Nevado-FiIábride domains, display analogous geological and petrographic features, as well as Ti, Zr, Y, Nb, trace elements contente All these aspects point to an alkaline intraplate magmatism, that can be related to a continental, tensional transcurrent zone