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dc.contributor.authorTeisseyre, Juliusz H.
dc.coverage.spatial14122 Åseral
dc.coverage.spatial14121 Austad
dc.coverage.spatial15124 Bygland
dc.coverage.spatial15123 Evje
dc.coverage.spatialEVJE OG HORNNES
dc.coverage.spatialBYGLAND
dc.date.accessioned2020-08-26T13:08:14Z
dc.date.available2020-08-26T13:08:14Z
dc.date.issued1970
dc.identifier.urihttps://hdl.handle.net/11250/2674918
dc.description.abstractThe area consists of Precambrian migmatic gneisses in which a group of banded gneisses (migmatic gneisses, sensu stricto) and a group of granite gneisses have been distinguished. Two stages of folding are readily distinguished, and it is possible to find some traces of an even older structure (F1). The F1 structures were refolded by a system of NW-SE folds (F2) and later by a system of E-W folds (F3). The second period of folding produced the most prominent structures, while the third episode is only of minor importance.
dc.language.isoeng
dc.relation.ispartofseriesNGU (266)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRUKTURGEOLOGI
dc.subjectPREKAMBRIUM
dc.subjectKARTLEGGING
dc.subjectPETROGRAFI
dc.subjectOMDANNING
dc.titleGeological investigations in the Byglandsfjorden-Gyvatn area. (The Precambrian rocks of the Telemark area in South Central Norway no. IX).
dc.typeJournal article
dc.description.localcode34886
dc.source.pagenumber206-229


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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