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

Impacto

Downloads

Downloads per month over past year



Arenas Martín, Ricardo and Nuez Pestana, Julio de la (2013) Características del metamorfismo hidrotermal del Complejo Plutónico de la Caldera de Taburiente (La Palma, Canarias). Geogaceta, 107 . pp. 64-74. ISSN 0213-683X

[thumbnail of Art05.pdf]
Preview
PDF
253kB

Official URL: http://www.rsehn.es/index.php?d=publicaciones



Abstract

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

Resumen (otros idiomas)

Item Type:Article
Uncontrolled Keywords:Hydrothermal metamorphism, Canary Islands
Palabras clave (otros idiomas):
Subjects:Sciences > Geology > Geochemistry
ID Code:70031
Deposited On:04 Feb 2022 07:02
Last Modified:04 Feb 2022 12:05

Origin of downloads

Repository Staff Only: item control page