dc.contributor.author | Strand, Trygve | |
dc.coverage.spatial | 17182 Vinstra | |
dc.coverage.spatial | NORD-FRON | |
dc.coverage.spatial | SEL | |
dc.date.accessioned | 2020-08-26T13:05:23Z | |
dc.date.available | 2020-08-26T13:05:23Z | |
dc.date.issued | 1967 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674885 | |
dc.description.abstract | A sequence of five separable formations of assumed Eocambrian to Cambrian and earliest Ordovician age are separated by a thrust-plane from the overlying Otta nappe. A lowermost formation of alternating schists and sandstones (often calcareous or dolomitic) and dolomites contains boulder-bearing schists, correlated with Eocambrian glacial horizon of south Norway (Moelv tillite). It is succeeded by a light feldspathic sandstone (\"light sparagmite\") a formation of alternating schists and sandstones (often calcareous or dolomitic), a thick pelitic sequence (phyllites) and an uppermost sandstone. In the eastern part of the area described on the rocks of this sequence are folded on NW-SE axes, two phases of folding have been ascertained, in the western part the structure is largely monoclinal with dips to NW to NNW. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU (251) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | SEDIMENTÆR BERGART | |
dc.subject | PETROGRAFI | |
dc.subject | SKIFER | |
dc.subject | STRATIGRAFI | |
dc.subject | KARTLEGGING | |
dc.subject | STRUKTURGEOLOGI | |
dc.title | Stratigraphy and structure of eocambrian and younger deposits in a part of the Gudbrandsdal valley district, south Norway. | |
dc.type | Journal article | |
dc.description.localcode | 34937 | |
dc.source.pagenumber | 93-106 | |