Emplazamiento tardihercínico de diques relacionados con el complejo plutónico de la Maladeta, Pirineo Axial

dc.contributor.authorGarcía Bellés, J.
dc.contributor.authorArranz, Enrique
dc.contributor.authorLago San José, Marceliano
dc.contributor.authorValenzuela Ríos, J. I.
dc.date.accessioned2015-04-09T12:22:08Z
dc.date.available2015-04-09T12:22:08Z
dc.date.issued1997
dc.description.abstractThe scope of this paper is the study of the chronological relationships between the Hercynian deformations and the emplacement of the Maladeta Plutonic Complex (M.P.C.) and related apical dykes. Both magmatic bodies were emplaced in epizonal levels (Cambrian to Carboniferous greenschists metasedimentary rocks) and crosscutting the structures (folds and cleavage) generated during the main Hercynian phase. The emplacement of the M.P.C. and the related dykes took place under a transpressive tectonic regime during Carboniferous timesen_US
dc.identifier.urihttp://hdl.handle.net/10272/10299
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.otherHercynianen_US
dc.subject.otherPlutonismen_US
dc.subject.otherPyreneesen_US
dc.subject.otherCalc-alkalineen_US
dc.subject.otherCarboniferousen_US
dc.subject.otherPostectonicen_US
dc.titleEmplazamiento tardihercínico de diques relacionados con el complejo plutónico de la Maladeta, Pirineo Axialen_US
dc.titleEmplacement of late-Hercynian dykes related to the Maladeta Plutonic Complex, Central Axial Zone, Pyreneeseng
dc.typejournal articleen_US
dspace.entity.typePublication

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