Características del metamorfismo hidrotermal del Complejo ·Plutónico de la Caldera de Taburiente (La Palma, Canarias)
- Ricardo Arenas Martín 1
- Julio de la Nuez Pestana 2
- 1 Departamento de Geología y PetroquImica U.C.M. Madrid.
- 2 Departamento de Edafología y Geología. Universidad de la Laguna. Tenerife.
ISSN: 0213-683X
Année de publication: 1987
Número: 3
Pages: 13-15
Type: Article
D'autres publications dans: Geogaceta
Résumé
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.