Emplazamiento de sills y diques del Pérmico superior en el 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.accessioned2015-03-26T11:19:35Z
dc.date.available2015-03-26T11:19:35Z
dc.date.issued1998
dc.description.abstractThe emplacement of basaltic sills and dykes outcropping in the Cinco Villas Massif (Western Pyrenees), northwards of the North-pyrenean fault, was controled by the hercynian main-phase cleavage (dykes) and by the orientation of three small half-graben permian basins (sills), unconformably overlain by the Buntsandstein conglomerates. Both types of magmatism are cogenetic and coevalen_US
dc.identifier.urihttp://hdl.handle.net/10272/10170
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.otherLate-Hercynianen_US
dc.subject.otherMagmatismen_US
dc.subject.otherPermianen_US
dc.subject.otherPyreneesen_US
dc.titleEmplazamiento de sills y diques del Pérmico superior en el Macizo de Cinco Villas (Pirineo Navarro)en_US
dc.titleUpper Permian emplacement of sills and dykes, in the Cinco Villas Massif (Navarra, Western Pyrenees)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 25, (1998)