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dc.contributor.authorKollung, Sigbjørn
dc.coverage.spatial21284 Junkerdal
dc.coverage.spatial21282 Graddis
dc.coverage.spatial21283 Lønsdal
dc.coverage.spatial21291 Sisovatn
dc.coverage.spatial22294 Skagmadal
dc.coverage.spatial22293 Låmivatnet
dc.coverage.spatial21294 Fauske
dc.coverage.spatial21293 Rognan
dc.coverage.spatial21292 Sulitjelma
dc.coverage.spatial21281 Balvatnet
dc.date.accessioned2020-08-26T11:02:55Z
dc.date.available2020-08-26T11:02:55Z
dc.date.issued1989
dc.identifier.urihttps://hdl.handle.net/11250/2674398
dc.description.abstractThe 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.isonor
dc.relation.ispartofseriesSkrifter (93)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectOFIOLITT
dc.subjectGRØNNSTEIN
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectMALMFOREKOMST
dc.subjectREGIONAL KARTLEGGING
dc.subjectSTRATIGRAFI
dc.titleSulitjelmafeltet. Berggrunnsgeologisk kart - M 1 : 100 000. Beskrivelse.
dc.typeMap
dc.description.localcode35684
dc.source.pagenumber1 - 47


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal