Resumen de Registro metamórfico de alta presión-baja temperatura en la unidad de Jubrique e imbricaciones de Benarrabá: (Cordillera Bético-Rifeña)

José Miguel Azañón Hernández, Juan Carlos Balanyá Roure, Víctor García Dueñas

• The presence of carpholitep seudomorphs and the kyanite-chloritoid-chlorite association in the Jubrique unitphy/iites and in the Benarrabá imbrications indicates metam rphic conditions of T < 450º C and P> 8 Kb. This means that these units were collisionally buried under crustal tectonic elements with a thickness of more than 20 Km.