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dc.contributor.authorSaintot, A.
dc.coverage.spatial17142 Kongsberg
dc.coverage.spatial17131 Siljan
dc.date.accessioned2020-07-15T07:45:39Z
dc.date.available2020-07-15T07:45:39Z
dc.date.issued2008
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664776
dc.description.abstractThe aim of this study was to determine the link between structural geology and the hydrogeological system of the Numedalen valley from Kongsberg to Hvittingfoss (Buskerud county) within the framework of the GEOS program. Three main geological units are presented: (1) Precambrian basement, (2) Late Caledonian sedimentary fold-and-thrust belt and (3) Premian Oslo Rift, all having a very low porosity and intrinsic permeability. In such medium, the groundwater flow is expected to be heterogeneous, anisotropic and controlled by fractures. (...)
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2008.018)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSPREKKESONE
dc.subjectSTRUKTURGEOLOGI
dc.subjectHYDROGEOLOGI
dc.titleBrittle tectonics in the Numedalen region. Insights into hydrogeology
dc.typeReport
dc.description.localcode54000
dc.source.pagenumber74 s.
dc.relation.project(301815) GEOS - Grunnvannsundersøkelser


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