%0 Journal Article %A Arenas Martín, Ricardo %A Nuez Pestana, Julio de la %T Características del metamorfismo hidrotermal del Complejo Plutónico de la Caldera de Taburiente (La Palma, Canarias) %D 2013 %@ 0213-683X %U https://hdl.handle.net/20.500.14352/34418 %X The Plutonic Complex cropping out in the Caldera de Taburiente is affected by a marked hydrothermal metamorphism, whose ITietamorphic peak conditions were reached in the upper-T part of the greenschist facies. A later retrogradation to the zeo/ite facies is related with the uplift of the ensemble from the ocean floor to the surface. Arenas, R. y Nuez, J. de la (1987): Características del metamorfismo hidrotermal del Complejo Plutónico de la Caldera de Taburiente (La Palma, Canarias). Geogaceta, 3, 13-15 %~