III. Kalksten fra Nordland
dc.contributor.author | Rekstad, Johan | |
dc.coverage.spatial | 20294 Bodø | |
dc.coverage.spatial | 20292 Misvær | |
dc.coverage.spatial | 21293 Rognan | |
dc.coverage.spatial | 18273 Sandnessjøen | |
dc.coverage.spatial | 18272 Nesna | |
dc.coverage.spatial | 18253 Bindal | |
dc.coverage.spatial | BODØ | |
dc.coverage.spatial | FAUSKE | |
dc.coverage.spatial | BINDAL | |
dc.coverage.spatial | DØNNA | |
dc.coverage.spatial | SALTDAL | |
dc.coverage.spatial | BRØNNØY | |
dc.coverage.spatial | NESNA | |
dc.date.accessioned | 2020-08-26T13:30:26Z | |
dc.date.available | 2020-08-26T13:30:26Z | |
dc.date.issued | 1914 | |
dc.identifier.uri | https://hdl.handle.net/11250/2675214 | |
dc.description.abstract | Some analyses of limestones from Northern Norway are given. They show that the percentage of carbonate of Magnesium (MgCO3) is small in several of these lime- stones. They may therefore be used in the industries of carbide and cellulose. The limestones of Northern Norway consist of varieties from almost pure carbo- nate of Calcium (CaCO3) to dolomite (CaCO3MgCO3). It was formerly a common belief that all the limestones of this region were too rich in carbonate of Magnesium for such uses, but that is not the case. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU (69) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | KALKSTEIN | |
dc.subject | SEDIMENTÆR BERGART | |
dc.subject | KARBONAT | |
dc.subject | OMDANNET BERGART | |
dc.subject | MARMOR | |
dc.subject | KJEMISK ANALYSE | |
dc.title | III. Kalksten fra Nordland | |
dc.type | Journal article | |
dc.description.localcode | 35608 | |
dc.source.pagenumber | 9 |
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