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Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/193556
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dc.contributor.authorGisbert Pinto, Guillem-
dc.contributor.authorGimeno Torrente, Domingo-
dc.date.accessioned2023-02-14T09:13:53Z-
dc.date.available2023-02-14T09:13:53Z-
dc.date.issued2013-
dc.identifier.issn0026-461X-
dc.identifier.urihttp://hdl.handle.net/2445/193556-
dc.description.abstractIn the Sulcis area (SW Sardinia, Italy) a thick OligoMiocene volcanic sequence formed during the drifting and rotation of Sardinia from the European continental margin to its current position. These volcanics originated by the combined effect of oceanic crust subduction under the Corsica-Sardinia microplate and increased extensional tectonics after 18 Ma-
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. 1177-1177-
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.classificationGeoquímica-
dc.subject.classificationRoques ígnies-
dc.subject.classificationSardenya (Itàlia)-
dc.subject.otherGeochemistry-
dc.subject.otherIgneous rocks-
dc.subject.otherSardinia (Italy)-
dc.titleUse of whole rock geochemistry for ignimbritic unit recognition: an example from the Sulcis area (SW Sardinia, Italy)-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec650979-
dc.date.updated2023-02-14T09:13:53Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
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