Granitoides peraluminosos y su relación con las rocas fuentes

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dc.contributor.authorDahlquist, Juan A.
dc.contributor.authorAlasino, Pablo H.
dc.contributor.authorGalindo Francisco, María Del Carmen
dc.date.accessioned2023-06-20T09:25:09Z
dc.date.available2023-06-20T09:25:09Z
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 environment
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/11478
dc.identifier.issn0213-683X
dc.identifier.officialurlhttp://www.sociedadgeologica.es/publicaciones_geogaceta.html
dc.identifier.urihttps://hdl.handle.net/20.500.14352/49428
dc.journal.titleGeogaceta
dc.language.isospa
dc.page.final214
dc.page.initial211
dc.publisherSociedad Geológica de España
dc.rights.accessRightsopen access
dc.subject.cdu552.3
dc.subject.keywordPeraluminous unit
dc.subject.keywordSource rocks
dc.subject.keywordGeochemical studies
dc.subject.keywordGeotectonic environment
dc.subject.ucmPetrología
dc.titleGranitoides peraluminosos y su relación con las rocas fuentes
dc.typejournal article
dc.volume.number38
dspace.entity.typePublication
relation.isAuthorOfPublicationf2fb71b6-b7fd-4fc6-bf39-d4de3ba5a67c
relation.isAuthorOfPublication.latestForDiscoveryf2fb71b6-b7fd-4fc6-bf39-d4de3ba5a67c
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