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dc.contributor.authorArenas, R.
dc.contributor.authorNuez, J. de la
dc.date.accessioned2020-07-03T13:43:22Z
dc.date.available2020-07-03T13:43:22Z
dc.date.issued1987
dc.identifier.urihttp://hdl.handle.net/10272/18419
dc.description.abstractThe 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 surfacees_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherHydrothermal metamorphismes_ES
dc.subject.otherCanary Islandses_ES
dc.titleCaracterísticas del metamorfismo hidrotermal del Complejo Plutónico de la Caldera de Taburiente (La Palma, Canarias)1987es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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