Azañón, José MiguelBalanyá, Juan CarlosGarcía Dueñas, V.2017-07-112017-07-111994http://hdl.handle.net/10272/13921The 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.spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/HP-LTmetamorphismCrustal thinningAipujarride ComplexRegistro metamorfico de alta presión-baja temperatura en la unidad de Jubrique e imbricaciones de Benarrabá (Cordillera Bético-Rifeña)High pressure-low temperature metamorphic record in the Jubrique unit and Benarrabá imbrications (Betic-Rift Cordillera)conference outputopen access