RT Journal Article
T1 Características del metamorfismo hidrotermal del Complejo Plutónico de la Caldera de Taburiente (La Palma, Canarias)
A1 Arenas Martín, Ricardo
A1 Nuez Pestana, Julio de la
AB 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
PB Sociedad Geológica de España
SN 0213-683X
YR 2013
FD 2013
LK https://hdl.handle.net/20.500.14352/34418
UL https://hdl.handle.net/20.500.14352/34418
LA spa
DS Docta Complutense
RD 14 dic 2025