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dc.contributor.authorReusch, Hans
dc.coverage.spatial19332 Gal'bajav'ri
dc.coverage.spatial19331 Suossjav'ri
dc.coverage.spatial20334 Iesjåkka
dc.coverage.spatial20333 Bæivasgiedde
dc.coverage.spatial20332 Galmatskai'di
dc.coverage.spatial20331 Karasjok
dc.coverage.spatialTANA
dc.coverage.spatialKAUTOKEINO
dc.coverage.spatial19333 Lappuluobbal
dc.coverage.spatial19334 Masi
dc.coverage.spatial19341 Cåkkaras'sa
dc.coverage.spatial19342 Iesjavri
dc.coverage.spatialKARASJOK
dc.coverage.spatialPORSANGER
dc.coverage.spatialALTA
dc.date.accessioned2020-08-26T13:20:11Z
dc.date.available2020-08-26T13:20:11Z
dc.date.issued1902
dc.identifier.urihttps://hdl.handle.net/11250/2675101
dc.description.abstractForkortet: The solid rock. In the region between Bjørnstad (NW corner of the map) and the first geological boundary line (dotted on the map) there are mostly sheared, quartzitic, feldsparbearing sandstone, lying more or less horizontally. Near to Boiabeska is a declivity represented on figs.2 and 3, page 10. On fig.3, the numerals indicate 1. gray, compact, somewhat schistose h\u00E4lleflinta with some phyllite; 2. reddish-gray sparagmite of a gneissic appearance; 3. red phyllite; 4. quartzitic sandstone; gray or greenish gray; 5. greenish gray phyllite with a slight fissility. The rock of Ravna and the neighbourhood (between the dotted lines on the map) is gneiss-granite, very much the same as the Archaean granites with parallel structuer in Southern Norway. At Kara- sjok and to the South and West of it the predominant rocks are altered sandstones, partly pure quartz sandstone, now appearing as quartzite; partly feldspar-bearing sandstone, now looking like gneissic rocks. Basic rocks, altered gabbro, amphibolite and amphibole schists occur there also. The rock at the gold washings at Sargijokk is probably a sheared gneiss, it is a light, fine-grained greenish-gray schist, rich in muscovite and chlorite. The rock is very much contorted as it seen in fig.1 on page 19 which represents a rock-face l m long.
dc.language.isonor
dc.relation.ispartofseriesNGU (36)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKVARTÆRGEOLOGI
dc.subjectMALMGEOLOGI
dc.subjectSTØRKNINGSBERGART
dc.subjectGULL
dc.subjectPETROGRAFI
dc.titleFra det indre af Finmarken
dc.typeJournal article
dc.description.localcode36054
dc.source.pagenumber64


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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