Geoquímica del magmatismo, Pérmico superior, del Macizo de Cinco Villas (Pirineo Navarro)

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dc.contributor.authorLasheras Adot, E.
dc.contributor.authorLago San José, Marceliano
dc.contributor.authorGarcía Bellés, J.
dc.contributor.authorArranz, Enrique
dc.date.accessioned2015-03-26T13:01:50Z
dc.date.available2015-03-26T13:01:50Z
dc.date.issued1998
dc.description.abstractThe chemical composition (whole rock) of Upper Permian basaltic sills and dolerite dykes outcropping in the Cinco Villas Massif (Western Pyrenees) allow to recognize: a) their basic, unevolved composition, b) their cogenetism, and c) their subalkaline to alkaline geochemical affinity. These features are similar to those of the Anayet-Ossau basaltic rocks, and suggest their relationship with a common basaltic event, related to post-orogenic extensional tectonicsen_US
dc.identifier.urihttp://hdl.handle.net/10272/10177
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGeochemistryen_US
dc.subject.otherMagmatismen_US
dc.subject.otherUpper Permianen_US
dc.subject.otherWestern Pyreneesen_US
dc.titleGeoquímica del magmatismo, Pérmico superior, del Macizo de Cinco Villas (Pirineo Navarro)en_US
dc.titleGeochemistry of Upper Permian magmatism in the Cinco Villas Massif (Navarra, Western Pyrenees)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 25, (1998)