Brittle tectonics in the Numedalen region. Insights into hydrogeology

dc.contributor.author	Saintot, A.
dc.coverage.spatial	17142 Kongsberg
dc.coverage.spatial	17131 Siljan
dc.date.accessioned	2020-07-15T07:45:39Z
dc.date.available	2020-07-15T07:45:39Z
dc.date.issued	2008
dc.identifier.issn	0800-3416
dc.identifier.uri	https://hdl.handle.net/11250/2664776
dc.description.abstract	The 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.iso	eng
dc.relation.ispartofseries	NGU-Rapport (2008.018)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	SPREKKESONE
dc.subject	STRUKTURGEOLOGI
dc.subject	HYDROGEOLOGI
dc.title	Brittle tectonics in the Numedalen region. Insights into hydrogeology
dc.type	Report
dc.description.localcode	54000
dc.source.pagenumber	74 s.
dc.relation.project	(301815) GEOS - Grunnvannsundersøkelser

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