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Jomaforekomstenes blokkvifter.

dc.contributor.authorOftedahl, Christoffer
dc.coverage.spatialRØYRVIK
dc.coverage.spatial19241 Jomafjellet
dc.coverage.spatialLIERNE
dc.date.accessioned2020-08-26T12:47:30Z
dc.date.available2020-08-26T12:47:30Z
dc.date.issued1957
dc.identifier.urihttps://hdl.handle.net/11250/2674659
dc.description.abstractThe Joma pyrite occurence contains some 15 million tons ore and crops out mostly under bogs with maximum ore zonewidth of 40 m. The surrounding morainic deposits have been investigated for ore boulders, in order to find the possible transport direction(s) of the Pleistocene glaciers. The observed ore boulders, plotted in Fig. 1, show a marked transposrt from east to west. A younger transport direction parallel to the Swedish border has produced a southern concentration of ore erratics.
dc.language.isonor
dc.relation.ispartofseriesNGU (200)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKVARTÆRGEOLOGI
dc.subjectBLOKKLETING
dc.subjectAVSETNING
dc.subjectBREBEVEGELSE
dc.subjectTRANSPORT
dc.subjectSULFID
dc.titleJomaforekomstenes blokkvifter.
dc.typeJournal article
dc.description.localcode35002
dc.source.pagenumber51-53


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