Show simple item record

dc.contributor.authorEnglund, Jens-Olaf
dc.coverage.spatial18183 Ringebu
dc.coverage.spatial18182 Imsdalen
dc.coverage.spatial18174 Fåvang
dc.coverage.spatial18171 Goppollen
dc.coverage.spatialGAUSDAL
dc.coverage.spatialØYER
dc.coverage.spatialRINGEBU
dc.date.accessioned2020-08-26T13:01:40Z
dc.date.available2020-08-26T13:01:40Z
dc.date.issued1966
dc.identifier.urihttps://hdl.handle.net/11250/2674834
dc.description.abstractRocks of latest Precambrian and Eocambrian age (the Sparagmite Group) dominate in the Fåvang area. In the western part they are overlain by Cambrian and Ordovician rocks. The stratigraphy of the sparagmite rocks (p. 58) is almost the same as in the classical area at lake Mjøsa. The rocks in the Fåvang area are supposed to be in an autochthonous or parautochthonous position. They are only slightly metamorphosed. The stratigraphy of the sparagmite rocks in the Fåvang area is from below: Eldstad sparagmite, Eldstad shale, Brøttum sparagmite, Brøttum shale and limestone (?), Biri conglomerate, Biri shale and limestone, Moelv sparagmite, Moelv conglomerate (tillite), Ekre shale, Vemdal sandstone (quartz-sandstone) and finally Svartskar shale (Lower Cambrian?). The Fåvang area belongs to the miogeosynclinal zone of the Caledonian Mountain Chain. The tectonic problems in this area, must therefore be seen in relation to the development of the Caledonides in central southeast Norway. The Vemdal sandstone with its typical imbricate structure (fig. 13 and fig. 18), was detached in the Ekre shale from the older sparagmites and moved in southerly or southeasterly direction.
dc.language.isonor
dc.relation.ispartofseriesNGU (238)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSEDIMENTOLOGI
dc.subjectSTRATIGRAFI
dc.subjectKARTLEGGING
dc.subjectPETROGRAFI
dc.subjectTEKTONIKK
dc.titleSparagmittgruppens bergarter ved Fåvang, Gudbrandsdalen. En sedimentlogisk og tektonisk undersøkelse.
dc.typeJournal article
dc.description.localcode35217
dc.source.pagenumber55-103 +


Files in this item

Thumbnail

This item appears in the following Collection(s)

  • Artikler [1063]
    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

Show simple item record

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