dc.contributor.author | Kollung, Sigbjørn | |
dc.coverage.spatial | 21284 Junkerdal | |
dc.coverage.spatial | 21282 Graddis | |
dc.coverage.spatial | 21283 Lønsdal | |
dc.coverage.spatial | 21291 Sisovatn | |
dc.coverage.spatial | 22294 Skagmadal | |
dc.coverage.spatial | 22293 Låmivatnet | |
dc.coverage.spatial | 21294 Fauske | |
dc.coverage.spatial | 21293 Rognan | |
dc.coverage.spatial | 21292 Sulitjelma | |
dc.coverage.spatial | 21281 Balvatnet | |
dc.date.accessioned | 2020-08-26T11:02:55Z | |
dc.date.available | 2020-08-26T11:02:55Z | |
dc.date.issued | 1989 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674398 | |
dc.description.abstract | The eugeoclinal rocks of the Sulitjelma region occup a large depression in the Norwegian Caldonodrd betwwen the Nasafjell tectonic window of Precambrian rocks in the south and the Tysfjord window in the north. The age of the rocks is thought to be Cambro-Silurian. The regionl metamophism is mainly in greenschist facies in the lower units, amphibolite facies in the Gasak Nappe and greenschist to amphibolite facies in the Fauske Nappe. Some of the largest sulphide deposits in Norway are located near Sulitjelma. The different types of mineralizations occurring in the region are briefly described. | |
dc.language.iso | nor | |
dc.relation.ispartofseries | Skrifter (93) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | OFIOLITT | |
dc.subject | GRØNNSTEIN | |
dc.subject | KALEDONSKE FJELLKJEDE | |
dc.subject | MALMFOREKOMST | |
dc.subject | REGIONAL KARTLEGGING | |
dc.subject | STRATIGRAFI | |
dc.title | Sulitjelmafeltet. Berggrunnsgeologisk kart - M 1 : 100 000. Beskrivelse. | |
dc.type | Map | |
dc.description.localcode | 35684 | |
dc.source.pagenumber | 1 - 47 | |