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dc.contributor.authorStarmer, Ian C.
dc.coverage.spatial17144 Flesberg
dc.date.accessioned2020-08-26T13:19:03Z
dc.date.available2020-08-26T13:19:03Z
dc.date.issued1979
dc.identifier.urihttps://hdl.handle.net/11250/2675081
dc.description.abstractThis major boundary is shown to be defined not by the traditional \"Friction Breccia\", but by a much earlier and more extensive mylonite zone. The mylonitisation was produced by a complex westward upthrust of the Kongsberg Series over the Telemark Series; both blocks had a common history thereafter. Spatial and chronological relationships between the upthrusting,, an extensive series of gabbroic intrusions and an increased heat flow, suggest association with major crust- mantle processes. The only major bend in the Kongsberg Series margin occurs in this area and in its location and development are explained.
dc.language.isoeng
dc.relation.ispartofseriesNGU (351)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectTEKTONIKK
dc.subjectMYLONITT
dc.subjectPREKAMBRIUM
dc.subjectSTRUKTURGEOLOGI
dc.subjectKARTLEGGING
dc.titleThe Kongsberg Series margin and its major bend in the Flesberg area, Numedal, Buskerud.
dc.typeJournal article
dc.description.localcode36261
dc.source.pagenumber99-120


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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