dc.contributor.author | Reusch, Hans | |
dc.coverage.spatial | 15322 Altevatn | |
dc.coverage.spatial | 15343 Tromsø | |
dc.coverage.spatial | 16343 Lyngen | |
dc.coverage.spatial | 13331 Gryllefjord | |
dc.coverage.spatial | KÅFJORD | |
dc.coverage.spatial | LYNGEN | |
dc.coverage.spatial | DYRØY | |
dc.coverage.spatial | SØRREISA | |
dc.coverage.spatial | SENJA | |
dc.coverage.spatial | BARDU | |
dc.coverage.spatial | TROMSØ | |
dc.coverage.spatial | MÅLSELV | |
dc.coverage.spatial | BALSFJORD | |
dc.date.accessioned | 2020-08-26T13:26:07Z | |
dc.date.available | 2020-08-26T13:26:07Z | |
dc.date.issued | 1891 | |
dc.identifier.uri | https://hdl.handle.net/11250/2675175 | |
dc.description.abstract | Forkortet: 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.iso | nor | |
dc.relation.ispartofseries | NGU (4) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | STØRKNINGSBERGART | |
dc.subject | PETROGRAFI | |
dc.subject | SEDIMENTÆR BERGART | |
dc.subject | KVARTÆRGEOLOGI | |
dc.subject | MALMGEOLOGI | |
dc.subject | OMDANNET BERGART | |
dc.title | Nogle bemerkninger om Tromsø amts geologi. (Efter Karl Pettersens arbeider) | |
dc.type | Journal article | |
dc.description.localcode | 36217 | |
dc.source.pagenumber | 112-119 | |