Resumen de Características del metamorfismo hidrotermal del Complejo ·Plutónico de la Caldera de Taburiente (La Palma, Canarias)

Ricardo Arenas Martín, Julio de la Nuez Pestana

• 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.