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dc.contributor.authorReusch, Hans
dc.coverage.spatial15322 Altevatn
dc.coverage.spatial15343 Tromsø
dc.coverage.spatial16343 Lyngen
dc.coverage.spatial13331 Gryllefjord
dc.coverage.spatialKÅFJORD
dc.coverage.spatialLYNGEN
dc.coverage.spatialDYRØY
dc.coverage.spatialSØRREISA
dc.coverage.spatialSENJA
dc.coverage.spatialBARDU
dc.coverage.spatialTROMSØ
dc.coverage.spatialMÅLSELV
dc.coverage.spatialBALSFJORD
dc.date.accessioned2020-08-26T13:26:07Z
dc.date.available2020-08-26T13:26:07Z
dc.date.issued1891
dc.identifier.urihttps://hdl.handle.net/11250/2675175
dc.description.abstractForkortet: This paper contains an explanation of the points where Pettersen differs from Dahll regarding the supposed Cambrian-Silurian schists. The illustrations p. 114, 115 are from the great mountain chain of gabbro to the West of the Lyngen fiord. The illustration p. 118 is from the schist country.
dc.language.isonor
dc.relation.ispartofseriesNGU (4)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTØRKNINGSBERGART
dc.subjectPETROGRAFI
dc.subjectSEDIMENTÆR BERGART
dc.subjectKVARTÆRGEOLOGI
dc.subjectMALMGEOLOGI
dc.subjectOMDANNET BERGART
dc.titleNogle bemerkninger om Tromsø amts geologi. (Efter Karl Pettersens arbeider)
dc.typeJournal article
dc.description.localcode36217
dc.source.pagenumber112-119


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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