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dc.contributor.authorEnglund, Jens-Olaf
dc.coverage.spatial18174 Fåvang
dc.coverage.spatial18183 Ringebu
dc.coverage.spatialRINGEBU
dc.coverage.spatialSØR-FRON
dc.coverage.spatial18182 Imsdalen
dc.coverage.spatialNORD-FRON
dc.coverage.spatial17182 Vinstra
dc.date.accessioned2020-08-26T13:10:58Z
dc.date.available2020-08-26T13:10:58Z
dc.date.issued1973
dc.identifier.urihttps://hdl.handle.net/11250/2674962
dc.description.abstractThe Ringebu-Vinstra district, Gudbrandsdalen, is one in which several of the main structural units in Southern Norway come together. Essentially, the rocks belong to three main tectonic units: 1. Parautochthonous rocks of the Hedmark Group of latest Precambrian and Eocambrian age with overlying Cambro-Ordovician deposits. 2. Allochthonous sedimentary rocks, which can be correlated with parts of the Hedmark Group and the Cambro-Ordovician, corresponding to the Kvitvola nappe occurring in Østerdalen and in Engerdalen. 3. Crystalline rocks of the Caledonian overthrust massifs, which in places are overlain by sedimentary rocks - the Jotun nappe. At Feforkampen the crystalline rocks with their cover of sedimentary rocks most probably correspond to the Valdres nappe. The Espedalen massif and the outlier of crystalline rocks in Valsfjell could also belong to the Valdres nappe. The sedimentary rocks from the present district are treated from a lithostratigraphical and petrographical point of view. The structural evolution of the Ringebu-Vinstra district has been complex with four major phases of deformation (D1-D4). The first phase of deformation involved the thrusting of the Jotun nappe-Valdres nappe and the Kvitvola nappe with minor thrusting of the parauthochthonous Vangsås Formation.
dc.language.isoeng
dc.relation.ispartofseriesNGU (293)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRUKTURGEOLOGI
dc.subjectGEOKRONOLOGI
dc.subjectSEDIMENTÆR BERGART
dc.subjectPETROGRAFI
dc.subjectKARTLEGGING
dc.subjectSTRATIGRAFI
dc.titleStratigraphy and structure of the Ringebu - Vinstra district, Gudbrandsdalen; with a short analysis of the western part of the sparagmite region.
dc.typeJournal article
dc.description.localcode36293
dc.source.pagenumber1-58 + ka


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