dc.contributor.author | Olesen, Odleiv | |
dc.contributor.author | Longva, Oddvar | |
dc.contributor.author | Bargel, Terje | |
dc.contributor.author | Nordgulen, Øystein | |
dc.contributor.author | Ottesen, Dag | |
dc.coverage.spatial | RØST | |
dc.coverage.spatial | VESTVÅGØY | |
dc.coverage.spatial | FLAKSTAD | |
dc.coverage.spatial | MOSKENES | |
dc.coverage.spatial | VÅGAN | |
dc.coverage.spatial | VÆRØY | |
dc.date.accessioned | 2020-07-15T07:50:43Z | |
dc.date.available | 2020-07-15T07:50:43Z | |
dc.date.issued | 2005 | |
dc.identifier.issn | 0800-3416 | |
dc.identifier.uri | https://hdl.handle.net/11250/2664958 | |
dc.description.abstract | (Forkortet)\rThe geology of the Lofoten region has been described with the aim of assessing whether or not the area would qualify as a candidate for the World Heritage List based on its natural properties.\rThe Lofoten archipelago consists mainly of Palaeoproterozoic rocks, including paragneisses and younger plutons (ca 1800 Ma) of the anorthosite-mangerite-charnokite-granite (AMCG) suite. The Precambiran basement of the Lofoten and the adjoining Vesterålen islands is part of a NNE-trending basement high that is overlain to the east by a stack of allochthonous nappes occupying the central axis of the Scandinavian Caledonides. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU-Rapport (2005.086) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | FJORD | |
dc.subject | BRE | |
dc.subject | GEOFYSIKK | |
dc.subject | GEOMORFOLOGI | |
dc.title | A preliminary study of Lofoten as a potential World Heritage Site based on natural criteria | |
dc.type | Report | |
dc.description.localcode | 52637 | |
dc.source.pagenumber | 27 s. | |
dc.relation.project | (312200) Lofoten; geofaglig vurdering av verdensarvområde | |