Vis enkel innførsel

dc.contributor.authorBinns, R.E.
dc.contributor.authorMatthews, D.W.
dc.contributor.authorChroston, P.N.
dc.coverage.spatial15352 Helgøy
dc.coverage.spatial16353 Karlsøy
dc.date.accessioned2020-08-26T13:19:47Z
dc.date.available2020-08-26T13:19:47Z
dc.date.issued1980
dc.identifier.urihttps://hdl.handle.net/11250/2675094
dc.description.abstractForkortet: Presumed Precambrian, quartzo-feldspathic gneisses on Vanna, northern Norway, are overlain by two formations of arkosic sandstone and siltstone, the Tinn- vatn and Bukkheia formations. The gneiss\/sedimentary sequence boundary is an undulating primary unconformity. Bedforms and sedimentary structures suggest that the two formations are fluviatile-deltaic and shallow-marine, respectively Diorite sheets intrude the upper formation. The sedimentary sequence is slightly metamorphosed and has been affected by at least three deformation episodes. Its age is discussed.
dc.language.isonor
dc.relation.ispartofseriesNGU (359)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPREKAMBRIUM
dc.subjectSEDIMENTÆR BERGART
dc.subjectOMDANNING
dc.subjectGEOKRONOLOGI
dc.subjectKARTLEGGING
dc.titleLow-grade sediments on Precambrian gneiss in Vanna, Troms, Northern Norway
dc.typeJournal article
dc.description.localcode36252
dc.source.pagenumber61-70


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

  • Artikler [1064]
    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

Vis enkel innførsel

Navngivelse 4.0 Internasjonal
Med mindre annet er angitt, så er denne innførselen lisensiert som Navngivelse 4.0 Internasjonal