Características mineralógicas de una sóvita pirofanítica de la Pta. del Peñón Blanco, Fuerteventura, Canarias

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dc.contributor.authorAhijado, A.
dc.date.accessioned2019-05-29T10:40:18Z
dc.date.available2019-05-29T10:40:18Z
dc.date.issued1992
dc.description.abstractA carbonite vein composed by caldte and pyrophanite is described. Pyrophanite, a very unusual mineral phase in this kind of rocks is formed at low temperatures. This vein is classified as a late carbonatitees_ES
dc.identifier.urihttp://hdl.handle.net/10272/16325
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.otherPyrophanitees_ES
dc.subject.otherCarbonatitees_ES
dc.subject.otherMineralogyes_ES
dc.subject.otherCanary Islandses_ES
dc.titleCaracterísticas mineralógicas de una sóvita pirofanítica de la Pta. del Peñón Blanco, Fuerteventura, Canariases_ES
dc.titleMineralogical features oía pyrophanite sóvite from Pta. del Peñón Blanco, Fuerteventuraeng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 12, (1992)