Arenas Martín, RicardoNuez Pestana, Julio de la2023-06-192023-06-1920130213-683Xchrome-extension://efaidnbmnnnibpcajpcglclefindmkaj/viewer.html?pdfurl=https%3A%2F%2Fsge.usal.es%2Farchivos%2Fgeogacetas%2FGeo03%2FArt05.pdf&clen=253486&chunk=truehttps://hdl.handle.net/20.500.14352/34418The 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, 13-15spajournal articlehttp://www.rsehn.es/index.php?d=publicacionesopen access551.25Hydrothermal metamorphismCanary IslandsGeoquímica2503 Geoquímica