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Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/193585
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dc.contributor.authorGaperini, D.-
dc.contributor.authorGisbert Pinto, Guillem-
dc.contributor.authorGimeno Torrente, Domingo-
dc.contributor.authorAulinas Juncà, Meritxell-
dc.contributor.authorMacera, P.-
dc.contributor.authorBosch, D.-
dc.date.accessioned2023-02-14T10:34:43Z-
dc.date.available2023-02-14T10:34:43Z-
dc.date.issued2013-07-01-
dc.identifier.issn0026-461X-
dc.identifier.urihttp://hdl.handle.net/2445/193585-
dc.description.abstractThe Neogene volcanism in NE Spain, which is related to the rift-type extensional tectonics affecting the eastern margin of Iberia since late Oligocene, is well represented in the basalts and basanites from the Garrotxa Volcanic Field (GVF).-
dc.format.extent1 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherMineralogical Society-
dc.relation.isformatofReproducció del document publicat a: https://doi.org/10.1180/minmag.2013.077.5.7-
dc.relation.ispartofMineralogical Magazine, 2013, vol. 77, num. 5, p. 1146-1146-
dc.relation.urihttps://doi.org/10.1180/minmag.2013.077.5.7-
dc.rights(c) Mineralogical Society, 2013-
dc.sourceArticles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)-
dc.subject.classificationVolcans-
dc.subject.classificationVulcanisme-
dc.subject.classificationMantell terrestre-
dc.subject.classificationGarrotxa (Catalunya)-
dc.subject.otherVolcanoes-
dc.subject.otherVolcanism-
dc.subject.otherMantle of the earth-
dc.subject.otherGarrotxa (Catalonia)-
dc.titleMantle source heterogeneity beneath the Garrotxa Volcanic Field (NE Spain)-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec638971-
dc.date.updated2023-02-14T10:34:43Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
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