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dc.contributor.authorBjørlykke, Knut
dc.coverage.spatial23353 Varangerbotn
dc.coverage.spatial23352 Nesseby
dc.date.accessioned2020-08-26T13:05:28Z
dc.date.available2020-08-26T13:05:28Z
dc.date.issued1967
dc.identifier.urihttps://hdl.handle.net/11250/2674887
dc.description.abstractThe Bigganjargga Tillite (Reusch moraine) of N. Norway rests on a striated surface of the underlying sandstone (Tana Group). This unconformity can be followed on both sides of the Varangerfjord and can be correlated with a similar slight angular unconformity below the Lower Tillite (Smalfjord Tillite) at Tana (Føyn 1937). The described sections through the latest Precambrian and Eocambrian of N. Norway show many lithological similarities to the corresponding sections in S. Norway and Scotland. The palaeoclimatic implications of the regional distribution of Eocambrian tillites are discussed, and it is concluded that the Eocambrian glaciation probably was more extensive than any other known glaciation.
dc.language.isoeng
dc.relation.ispartofseriesNGU (251)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectPREKAMBRIUM
dc.subjectMORENE
dc.subjectGLASIALGEOLOGI
dc.subjectSEDIMENTÆR BERGART
dc.subjectSTRATIGRAFI
dc.titleThe Eocambrian "Reusch moraine" at Bigganjargga and the geology around Varangerfjord, Northern Norway.
dc.typeJournal article
dc.description.localcode34932
dc.source.pagenumber18-44


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