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Age and metamorphic conditions of the Tjeliken garnet – phengite gneiss (Swedish Caledonides)

creativeworkseries.issn2299-8004
dc.contributor.authorAndersson, Barbro
dc.date.available2017-08-22T10:46:42Z
dc.date.issued2015
dc.description.abstractEroded down to mid-crustal level the Scandinavian Caledonides offer a unique opportunity to study the interior of a mountain chain and provide insight of processes active during orogenesis.en
dc.description.placeOfPublicationKraków
dc.description.versionwersja wydawnicza
dc.identifier.doihttp://dx.doi.org/10.7494/geol.2015.41.1.55
dc.identifier.eissn2353-0790pl
dc.identifier.issn2299-8004pl
dc.identifier.nukatdd2015318112
dc.identifier.urihttps://repo.agh.edu.pl/handle/AGH/45916
dc.language.isoeng
dc.publisherWydawnictwa AGH
dc.relation.ispartofGeology, Geophysics & Environment
dc.rightsAttribution 4.0 International
dc.rights.accessotwarty dostęp
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/legalcode
dc.subjectmountainen
dc.subjectchainen
dc.subjectOrogenesisen
dc.titleAge and metamorphic conditions of the Tjeliken garnet – phengite gneiss (Swedish Caledonides)en
dc.title.relatedGeology, Geophysics & Environment
dc.typeartykuł
dspace.entity.typePublication
publicationissue.issueNumberNo. 1
publicationissue.paginationpp. 55-56
publicationvolume.volumeNumberVol. 41
relation.isJournalIssueOfPublication937aa5fa-1848-443b-880d-878793fd31ef
relation.isJournalIssueOfPublication.latestForDiscovery937aa5fa-1848-443b-880d-878793fd31ef
relation.isJournalOfPublicationb0bafc1e-4fd1-4ff1-822c-c1a78e14c892

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