Características y procesos postemplazamiento de la ignimbrita de la playa de San Juan (Tenerife)

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dc.contributor.authorCoello Bravo, Juan Jesús
dc.contributor.authorIzquierdo, F. J.
dc.date.accessioned2019-05-29T11:12:36Z
dc.date.available2019-05-29T11:12:36Z
dc.date.issued1992
dc.description.abstractThe Playa de San Juan Ignimbrite is a peralkaline pyroclastic flow that shows important facies variations depending on its emplacement position. The ignimbrite is strongly welded, where slopes exceed about 2CP dipping fiamme, lamination and others structures indicate secondaty flow simultaneous with compaction and coolinges_ES
dc.identifier.urihttp://hdl.handle.net/10272/16326
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherIgnimbritees_ES
dc.subject.otherWeldinges_ES
dc.subject.otherSecondary flowes_ES
dc.titleCaracterísticas y procesos postemplazamiento de la ignimbrita de la playa de San Juan (Tenerife)es_ES
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 12, (1992)