Granitoides peraluminosos y su relación con las rocas fuentes

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dc.contributor.authorDahlquist, J. A.
dc.contributor.authorAlasino, P. H.
dc.contributor.authorGalindo, Carmen
dc.date.accessioned2014-08-08T09:36:46Z
dc.date.available2014-08-08T09:36:46Z
dc.date.issued2005
dc.description.abstractComparative compositional studies between two peraluminous unit with magmatic andalucite and cordierite indicate that they were produced by partial melting of two differents metasedimentary source rocks. We conclude that geochemical studies from peraluminous unit contributes to define the source rocks and to constrain the pre-orogenic geotectonic environmenten_US
dc.identifier.urihttp://hdl.handle.net/10272/8721
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.otherPeraluminous uniten_US
dc.subject.otherSource rocksen_US
dc.subject.otherGeochemical studiesen_US
dc.subject.otherGeotectonic environmenten_US
dc.titleGranitoides peraluminosos y su relación con las rocas fuentesen_US
dc.titlePeraluminous granitoids and their relationship with the source rockseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 38, (2005)