@conference{10272/13921,
year = {1994},
url = {http://hdl.handle.net/10272/13921},
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.},
publisher = {Sociedad Geológica de España},
title = {Registro metamorfico de alta presión-baja temperatura en la unidad de Jubrique e imbricaciones de Benarrabá (Cordillera Bético-Rifeña)},
title = {High pressure-low temperature metamorphic record in the Jubrique unit and Benarrabá imbrications (Betic-Rift Cordillera)},
author = {Azañón, José Miguel and Balanyá, Juan Carlos and García Dueñas, V.},
}