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dc.contributor.authorBanks, Nigel L.
dc.coverage.spatial20341 Hal'kavarri
dc.date.accessioned2020-08-26T13:10:18Z
dc.date.available2020-08-26T13:10:18Z
dc.date.issued1973
dc.identifier.urihttps://hdl.handle.net/11250/2674953
dc.description.abstractThe increasing abundance of trace fossils in the ?late Precambrian to Lower Cambrian sediments of the Dividal Group is comparable with that found in the laterally equivalent but much thicker succession to the east and provides further evidence of the gradual but rapid development of metazoan life at that time.
dc.language.isoeng
dc.relation.ispartofseriesNGU (288)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectFOSSIL
dc.subjectSTRATIGRAFI
dc.subjectGEOKRONOLOGI
dc.subjectPALEONTOLOGI
dc.subjectPETROGRAFI
dc.subjectSEDIMENTÆR BERGART
dc.titleTrace fossils in the Halkkavarre section of the Dividal Group (?late Precambrian - Lower Cambrian), Finnmark.
dc.typeJournal article
dc.description.localcode35257
dc.source.pagenumber1-6


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal