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Structure of the synkinematic Lys pluton (Pyrenean Axial Zone)

dc.contributor.authorHilario, Asier
dc.contributor.authorAranguren, A.
dc.contributor.authorTubía, José María
dc.contributor.authorPinotti, Lucio P.
dc.date.accessioned2014-10-30T12:23:00Z
dc.date.available2014-10-30T12:23:00Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10272/9040
dc.description.abstractFrom the structural study (using field, microstructural and anisotropy of magnetic susceptibility data) of the central traverse across the Lys pluton (Pyrenean Axial Zone), w'e propose that the emplacement of this pluton is synkinematic with the Variscan deformation of the Cambro-Ordovician schists that form its northern envelop. The late emplacement events involve a dextral transpressional deformation leading to the development of the Esera-Gistain and Caillaouas ductile shear zones. These Variscan shear zones were reactivated during the Pyrenean orogenyen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherLys plutonen_US
dc.subject.otherPyreneesen_US
dc.subject.otherStructureen_US
dc.subject.otherSynkinematic emplacementen_US
dc.titleEstructura del pluton sincinematico de Lys (Zona Axial del Pirineo)en_US
dc.titleStructure of the synkinematic Lys pluton (Pyrenean Axial Zone)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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