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dc.contributor.authorGustavson, Magne
dc.coverage.spatial19253 Majavatn
dc.coverage.spatial19252 Børgefjellet
dc.coverage.spatial19251 Susendalen
dc.coverage.spatialGRANE
dc.coverage.spatialTRØNDELAG
dc.coverage.spatialRØYRVIK
dc.coverage.spatial19254 Svenningdal
dc.coverage.spatialNORDLAND
dc.coverage.spatialHATTFJELLDAL
dc.date.accessioned2020-08-26T13:11:06Z
dc.date.available2020-08-26T13:11:06Z
dc.date.issued1973
dc.identifier.urihttps://hdl.handle.net/11250/2674964
dc.description.abstractThree main structural units are present: 1. The Precambrian (Svecofennokarelian) basement of the Børgefjell Window. \". Low grade (greenschist facies) Lower Paleozoic rocks belonging to the Seve-Køli Nappe Complex. 3. The higher grade (amphibolite facies) Helgeland Nappe, thrust on top of the low grade rocks. The bedrock lithologies within these units are briefly described. Metasediments, metavolcanics and intrusive igneous rocks are present in the Caledonian part of the sequence. Within the Precambrian, granite and granitic gneiss predominate but metasediments and rocks transitional between gneisses and the metasediments are common. The stratigraphical position of the Caledonian rocks is briefly discussed.
dc.language.isonor
dc.relation.ispartofseriesNGU; Skrifter (298 ; 8)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRATIGRAFI
dc.subjectSTRUKTURGEOLOGI
dc.subjectPETROGRAFI
dc.subjectKVARTÆRGEOLOGI
dc.subjectKARTLEGGING
dc.subjectGEOKRONOLOGI
dc.titleBørgefjell. Beskrivelse til det berggrunnsgologiske gradteigskart J.19 - 1: 100 000
dc.typeJournal article
dc.description.localcode36176
dc.source.pagenumber43 + kart


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