Características del metamorfismo hidrotermal del Complejo Plutónico de la Caldera de Taburiente (La Palma, Canarias)1987
The Plutonic Complex cropping out in the Caldera de Taburiente is affected by a marked hydrothermal metamorphism, whose metamorphic peak conditions were reached in the upper-T part of the greenschist facies. A later retrogradation to the zeolite facies is related with the uplift of the ensemble from...
| Autores: | , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 1987 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18419 |
| Acceso en línea: | http://hdl.handle.net/10272/18419 |
| Access Level: | acceso abierto |
| Palabra clave: | Hydrothermal metamorphism Canary Islands |
| Sumario: | The Plutonic Complex cropping out in the Caldera de Taburiente is affected by a marked hydrothermal metamorphism, whose metamorphic peak conditions were reached in the upper-T part of the greenschist facies. A later retrogradation to the zeolite facies is related with the uplift of the ensemble from the ocean floor to the surface |
|---|