2026-06-27T10:23:00Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/344182023-08-26T07:32:37Zcom_20.500.14352_14col_20.500.14352_15

Arenas Martín, Ricardo Nuez Pestana, Julio de la 2023-06-19T13:46:57Z 2023-06-19T13:46:57Z 2013 0213-683X chrome-extension://efaidnbmnnnibpcajpcglclefindmkaj/viewer.html?pdfurl=https%3A%2F%2Fsge.usal.es%2Farchivos%2Fgeogacetas%2FGeo03%2FArt05.pdf&clen=253486&chunk=true https://hdl.handle.net/20.500.14352/34418 http://www.rsehn.es/index.php?d=publicaciones 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 spa open access Características del metamorfismo hidrotermal del Complejo Plutónico de la Caldera de Taburiente (La Palma, Canarias) journal article