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dc.contributor.authorNicholson, Robin
dc.coverage.spatial22293 Låmivatnet
dc.date.accessioned2020-08-26T13:03:40Z
dc.date.available2020-08-26T13:03:40Z
dc.date.issued1967
dc.identifier.urihttps://hdl.handle.net/11250/2674856
dc.description.abstractThe common minor scale kink-zones of upper levels of the Furulund schists of eastern Norwegian Sulitjelma generally do not occur in conjugate pairs: usually only the member with northwest dipping axial plane is developed although at lower levels rarely both conjugate pairs and single members occur. The kink-zones fit the simple shear mechanism of development proposed by Dewey and Roberts. The upper kink-zones are characterised by a well-developed metamorphic differentiation structure resulting fron the juxtaposition of zones alternately rich in mica and quartz. In many of the kink-zones the mica-rich zones are bent by smaller scale folds unknown elsewhere in the region but which are geometrically conjugate to the minor-scale structure in which they lie. Although they clearly are later than the kink-zones it is judged that they are directly related to them.
dc.language.isoeng
dc.relation.ispartofseriesNGU (247)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRUKTURGEOLOGI
dc.subjectFYLLITT
dc.subjectOMDANNET BERGART
dc.subjectFOLDNING
dc.titleOn kink-zone development and metamorphic differentiation in the low-grade schists of Norwegian Sulitjelma.
dc.typeJournal article
dc.description.localcode34908
dc.source.pagenumber133-146


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