Petrología, geoquímica y emplazamiento de diques de composición granodiorítica al sur del complejo plutónico de la Maladeta. (Zona Axial Pirenaica)

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dc.contributor.authorGarcía Bellés, J.
dc.contributor.authorLago San José, Marceliano
dc.contributor.authorArranz, Enrique
dc.contributor.authorValenzuela Ríos, J. I.
dc.date.accessioned2015-04-29T08:54:42Z
dc.date.available2015-04-29T08:54:42Z
dc.date.issued1997
dc.description.abstractA set of granodioritic dykes, related to the main intrusive episode of the Maladeta Plutonic Complex, is studied. These dykes, that follow the main cleavage strike, cut across deformed Paleozoic country rocks. Their composition (mineralógicaI and geochemical) is calk-alkaline and their emplacement was controlled by the previous hercynlc structure and by a transtensive regime during their interval of emplacementen_US
dc.identifier.urihttp://hdl.handle.net/10272/10463
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.otherDykesen_US
dc.subject.otherGranodioriticen_US
dc.subject.otherCalk-alkalineen_US
dc.subject.otherMaladetaen_US
dc.subject.otherAxial Pyreneesen_US
dc.titlePetrología, geoquímica y emplazamiento de diques de composición granodiorítica al sur del complejo plutónico de la Maladeta. (Zona Axial Pirenaica)en_US
dc.titlePetrology, geochemistry and emplacement of granodioritic dykes south of Maladeta plutonic complex (Pyrenean Axial Zone)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 23, (1997)