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dc.contributor.authorBjørlykke, Knut O.
dc.coverage.spatial17182 Vinstra
dc.coverage.spatial18184 Atnsjøen
dc.coverage.spatial19162 Tangen
dc.coverage.spatial19161 Løten
dc.coverage.spatialNORDRE LAND
dc.coverage.spatialGJØVIK
dc.coverage.spatialLILLEHAMMER
dc.coverage.spatialELVERUM
dc.coverage.spatialINNLANDET
dc.coverage.spatialTRØNDELAG
dc.coverage.spatialVESTLAND
dc.coverage.spatialVIKEN
dc.coverage.spatialRINGSAKER
dc.coverage.spatialHAMAR
dc.coverage.spatialSTANGE
dc.coverage.spatialVANG OPPLAND
dc.coverage.spatialTRYSIL
dc.coverage.spatialÅMOT
dc.date.accessioned2020-08-26T13:25:07Z
dc.date.available2020-08-26T13:25:07Z
dc.date.issued1905
dc.identifier.urihttps://hdl.handle.net/11250/2675171
dc.description.abstractForkortet: By Central Norway is here meant the three great valleys Østerdal, Gudbrandsdal and Valdres with their surroundings. In the district around lake Mjøsa there are opportunities for studying the differnt characteristics of the structure of the earth's crust in the different kinds of soft rocks which the Silurian etages or groups of strata consist and in the thicker and harder beds of sand- stone and sparagmite; in the former the foldings are characteristic, in the latter fracture planes or faults; inversion are common, but the greater overthrusts have not been detected (p.31). The pre-Cambrian strata in the Mjøsa district consist of the following divisions from above: (Ollenellus shales)\/ Quartz-sandstone-goup\/. The light (colored) Sparagmite with conglomerate.\/Birikalk (limestone)\/Biri.conglomerate\/.The Dark Sparagmite and shales.
dc.language.isonor
dc.relation.ispartofseriesNGU (39)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectSTRUKTURGEOLOGI
dc.subjectOMDANNET BERGART
dc.subjectKARTLEGGING
dc.subjectSTRATIGRAFI
dc.subjectSTØRKNINGSBERGART
dc.titleDet centrale Norges fjeldbygning
dc.typeJournal article
dc.description.localcode36021
dc.source.pagenumber595


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