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Compositional differences between Besko and Otryt sandstones of the Krosno Beds (Oligocene) in Eastern part of the Silesian Tectonic Unit

creativeworkseries.issn2299-8004
dc.contributor.authorGodlewski, Paweł
dc.contributor.authorWendorff, Marek
dc.contributor.authorŚwiąder, Andrzej
dc.date.available2017-08-30T06:57:13Z
dc.date.issued2016
dc.description.abstractThe Krosno Formation (Oligocene) in the Silesian Tectonic Unit of the E part of the Polish Outer Carpathians is represented by two lithofacies called the Besko (or Lesko) and the Otryt facies.en
dc.description.placeOfPublicationKraków
dc.description.versionwersja wydawnicza
dc.identifier.doihttp://dx.doi.org/10.7494/geol.2016.42.1.73
dc.identifier.eissn2353-0790pl
dc.identifier.issn2299-8004pl
dc.identifier.nukatdd2016315070
dc.identifier.urihttps://repo.agh.edu.pl/handle/AGH/46832
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.subjectlithofaciesen
dc.subjectsedimentary featuresen
dc.subjectoutcropen
dc.titleCompositional differences between Besko and Otryt sandstones of the Krosno Beds (Oligocene) in Eastern part of the Silesian Tectonic Uniten
dc.title.relatedGeology, Geophysics & Environment
dc.typeartykuł
dspace.entity.typePublication
publicationissue.issueNumberNo. 1
publicationissue.paginationpp. 73-74
publicationvolume.volumeNumberVol. 42
relation.isAuthorOfPublication47f4ce80-bb5a-4070-b7bb-aefa66e0ddfa
relation.isAuthorOfPublication68b14a6e-435e-4557-bb6e-87fee07904fc
relation.isAuthorOfPublication.latestForDiscovery47f4ce80-bb5a-4070-b7bb-aefa66e0ddfa
relation.isJournalIssueOfPublicationcb82a9e9-66ad-489c-b571-b6aba087a786
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relation.isJournalOfPublicationb0bafc1e-4fd1-4ff1-822c-c1a78e14c892

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