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dc.contributor.authorMarstrander, Rolf
dc.coverage.spatial20274 Storforshei
dc.coverage.spatial20283 Blakkådal
dc.coverage.spatial19274 Sjona
dc.coverage.spatial19271 Mo i Rana
dc.coverage.spatialRANA
dc.coverage.spatial19282 Svartisen
dc.coverage.spatialRØDØY
dc.coverage.spatialMELØY
dc.coverage.spatial19283 Melfjorden
dc.date.accessioned2020-08-26T13:29:01Z
dc.date.available2020-08-26T13:29:01Z
dc.date.issued1911
dc.identifier.urihttps://hdl.handle.net/11250/2675198
dc.description.abstractForkortet: The glacier Svartisen is, next to Jostedals glacier, the largest in Norway, and one of the largest in Europe. The arctic Circle passes through its southern part. Wherever accessible, the underlying rocks are found to consist mainly of granite in the Western Plateau, or crystalline schists in the Eastern, to be traced to the so-called mica-schists-marble group, (probably of cambro- silurian age) to which the greater part of the crystalline schists in Nordland belongs. The crystalline schists must rather be described as a series of gneiss and mica-schists, containing all posssible variations of these two rocks,besid- es quartzites and bands of amphibolite. Specially prominent was the garnet- mica-schist; it was characteristic of the whole district.
dc.language.isonor
dc.relation.ispartofseriesNGU (59)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectOMDANNET BERGART
dc.subjectPETROGRAFI
dc.subjectGRANITT
dc.subjectKARTLEGGING
dc.subjectSTØRKNINGSBERGART
dc.subjectSEDIMENTÆR BERGART
dc.titleIV. Svartisen. Dens geologi
dc.typeJournal article
dc.description.localcode35920
dc.source.pagenumber31


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