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dc.contributor.authorRutter, E.H.
dc.contributor.authorMatthews, J.E.
dc.contributor.authorChaplow, R.
dc.coverage.spatial15213 Løkken
dc.date.accessioned2020-08-26T13:06:08Z
dc.date.available2020-08-26T13:06:08Z
dc.date.issued1968
dc.identifier.urihttps://hdl.handle.net/11250/2674898
dc.description.abstractThe paper describes the rock types and geological structure of the Løkken area, near Trondheim. The area lies on the inverted limb of a nappe structure overturned to the north-west. This structure has been coaxially refolded. Chlorite grade basic metavolcanics of the Støren Groupare perserved from erosion in the core of a synformal second fold, and are structurally underlain by younger sediments og the younger Hovin Group. Mica schists in the north, traditionally ascribed to the Cambrian Røros Group,are found to be, locally at last, equivalent to the Hovin Group sediments.
dc.language.isoeng
dc.relation.ispartofseriesNGU (255)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKARTLEGGING
dc.subjectFOLDNING
dc.subjectPETROGRAFI
dc.subjectSEDIMENTÆR BERGART
dc.subjectSTRUKTURGEOLOGI
dc.subjectSTØRKNINGSBERGART
dc.titleThe geology of the Løkken area, Sør-Trøndelag.
dc.typeJournal article
dc.description.localcode34947
dc.source.pagenumber21-36 + ka


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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