Use of whole rock geochemistry for ignimbritic unit recognition: an example from the Sulcis area (SW Sardinia, Italy)

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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.date.updated2023-02-14T09:13:53Z
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.identifier.idgrec650979
dc.identifier.issn0026-461X
dc.identifier.urihttps://hdl.handle.net/2445/193556
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.rights.accessRightsinfo:eu-repo/semantics/openAccess
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

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