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Kullblendeførende breksje ved Hof, Solør.

dc.contributor.authorHjelle, Audun
dc.contributor.authorBryn, Knut Ørn
dc.coverage.spatial20162 Flisa
dc.date.accessioned2020-08-26T12:51:56Z
dc.date.available2020-08-26T12:51:56Z
dc.date.issued1961
dc.identifier.urihttps://hdl.handle.net/11250/2674737
dc.description.abstractThe breccia has possibly connection with the Permian faults in Rendalen, farther north, and the coal blend is probably derived from the dark Cambrian shale, once deposited on the Precambrian peneplane. A number of minerals and a fine grained sediment, occurring in some cavities, are described.
dc.language.isonor
dc.relation.ispartofseriesNGU (213)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKULL
dc.subjectBREKSJE
dc.subjectMIKROSKOPERING
dc.subjectMINERALOGI
dc.subjectPETROGRAFI
dc.subjectGNEIS
dc.titleKullblendeførende breksje ved Hof, Solør.
dc.typeJournal article
dc.description.localcode35670
dc.source.pagenumber49-57


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