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

  1. Ricardo Arenas Martín 1
  2. Julio de la Nuez Pestana 2
  1. 1 Departamento de Geología y PetroquImica U.C.M. Madrid.
  2. 2 Departamento de Edafología y Geología. Universidad de la Laguna. Tenerife.
Zeitschrift:
Geogaceta

ISSN: 0213-683X

Datum der Publikation: 1987

Nummer: 3

Seiten: 13-15

Art: Artikel

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Andere Publikationen in: Geogaceta

Zusammenfassung

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.

Fuente de los datos: Dialnet