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.
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1987

Zenbakia: 3

Orrialdeak: 13-15

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

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.

Datuen iturria: Dialnet