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dc.contributor.authorAkselsen, John
dc.coverage.spatial19354 Vargsund
dc.coverage.spatial19363 Hammerfest
dc.date.accessioned2020-08-26T13:21:31Z
dc.date.available2020-08-26T13:21:31Z
dc.date.issued1982
dc.identifier.urihttps://hdl.handle.net/11250/2675128
dc.description.abstractThe metamorphic rocks of northeastern Seiland are predominantly Precambrian gneisses and schists. The Fagervik infracrustal complex, composed of tonalitic gneisses, constitutes a basement to the Late Precambrian-Cambrian Klubben Psammite Group, while the Precambrian Eidvågeid supracrustal sequence occurs as the uppermost allochtonous nappe. The Precambrian units contain evidence of Precambrian deformation and metamorphism. The subsequent Caledonian tectonism is characterized by two phases of deformation D1 and D2. A metamorphic climax occurred in the interkinematic period. D1 produced large isoclinal folds and large-scale translation of the nappes. The major D2 structure is large asymmetric synform, the Storbukt Synform, with a vergence towards the southeast.
dc.language.isoeng
dc.relation.ispartofseriesNGU (373)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSKIFER
dc.subjectOMDANNING
dc.subjectTEKTONIKK
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectGNEIS
dc.titlePrecambrian and Caledonian tectonometamorphic evolution of Northeastern Seiland, Finnmark, North Norway.
dc.typeJournal article
dc.description.localcode35592
dc.source.pagenumber45 - 61


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