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dc.contributor.authorSmelror, Morten
dc.contributor.authorSolbakk, Terje
dc.contributor.authorRindstad, Bjørn Ivar
dc.contributor.authorStuedal, Helle Vangen
dc.contributor.authorHårsaker, Karstein
dc.date.accessioned2021-02-08T14:25:48Z
dc.date.available2021-02-08T14:25:48Z
dc.date.created2020-10-25T17:55:37Z
dc.date.issued2020
dc.identifier.citationNorwegian Journal of Geology. 2020, 100, .en_US
dc.identifier.issn2387-5844
dc.identifier.urihttps://hdl.handle.net/11250/2726658
dc.description.abstractGraptolites and trace fossils typical of deep-water environments are found on phyllitic roofing slates kept in the collections of the Stjørdal Museum Værnes, Trøndelag. The slates probably come from abandoned local quarries in the Stjørdal and Lånke districts. The fossils from Lånke also include some graptolites and poorly preserved nautiloids stored at the NTNU Vitenskapsmuseet, Trondheim. The graptolites indicate a Katian age, while the trace fossil assemblages compare to similar assemblages reported from the Middle–Late Ordovician Vuddudalen and Lower Hovin groups and the mostly Silurian Ekne Group of the Central Norwegian Caledonides.en_US
dc.language.isoengen_US
dc.publisherGeological Society of Norwayen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleNotes on Ordovician graptolites, nautiloides and trace fossils from Lånke, Central Norwegian Caledonidesen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.source.volume100en_US
dc.source.journalNorwegian Journal of Geologyen_US
dc.source.issue2en_US
dc.identifier.doi10.17850/njg100-2-2
dc.identifier.cristin1842093
dc.description.localcode© Copyright the authors. This work is licensed under a Creative Commons Attribution 4.0 International License.en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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