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

Abstract

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.