Geology of the northernmost part of the Meråker area.

dc.contributor.author	Siedlecka, Anna
dc.contributor.author	Siedlecki, Stanislaw
dc.coverage.spatial	17222 Feren
dc.coverage.spatial	VERDAL
dc.coverage.spatial	MERÅKER
dc.date.accessioned	2020-08-26T13:03:00Z
dc.date.available	2020-08-26T13:03:00Z
dc.date.issued	1967
dc.identifier.uri	https://hdl.handle.net/11250/2674845
dc.description.abstract	Four 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.iso	eng
dc.relation.ispartofseries	NGU (245)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	PETROGRAFI
dc.subject	KARTLEGGING
dc.subject	STRATIGRAFI
dc.subject	STØRKNINGSBERGART
dc.subject	STRUKTURGEOLOGI
dc.subject	SEDIMENTÆR BERGART
dc.title	Geology of the northernmost part of the Meråker area.
dc.type	Journal article
dc.description.localcode	35198
dc.source.pagenumber	59-63

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