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dc.contributor.authorSiedlecka, Anna
dc.contributor.authorSiedlecki, Stanislaw
dc.coverage.spatial17222 Feren
dc.coverage.spatialVERDAL
dc.coverage.spatialMERÅKER
dc.date.accessioned2020-08-26T13:03:00Z
dc.date.available2020-08-26T13:03:00Z
dc.date.issued1967
dc.identifier.urihttps://hdl.handle.net/11250/2674845
dc.description.abstractFour lithostratigraphical groups comprising sedimentary and igneous rocks have been distinguished in the mapped area. There are conformities and gradual transition between all these groups. The rocks have been subjected to a low grade of metamorphism, being changed to metabasites and metasediments. They are folded, with fold axes trending approximately NNE. The lithological units form narrow elongated zones dipping to the west. In the eastern part of the area an asymmetrical syncline has been observed.
dc.language.isoeng
dc.relation.ispartofseriesNGU (245)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectKARTLEGGING
dc.subjectSTRATIGRAFI
dc.subjectSTØRKNINGSBERGART
dc.subjectSTRUKTURGEOLOGI
dc.subjectSEDIMENTÆR BERGART
dc.titleGeology of the northernmost part of the Meråker area.
dc.typeJournal article
dc.description.localcode35198
dc.source.pagenumber59-63


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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