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

• Ricardo Arenas Martín ^[2] ; Julio de la Nuez Pestana ^[1]
  1. [1] Universidad de La Laguna

     Universidad de La Laguna

     San Cristóbal de La Laguna, España

     
  2. [2] Departamento de Geología y PetroquImica U.C.M. Madrid.
• Localización: Geogaceta, ISSN 0213-683X, Nº. 3, 1987, págs. 13-15
• Idioma: español
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• Resumen

  • 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.