The geology of the Løkken area, Sør-Trøndelag.

dc.contributor.author	Rutter, E.H.
dc.contributor.author	Matthews, J.E.
dc.contributor.author	Chaplow, R.
dc.coverage.spatial	15213 Løkken
dc.date.accessioned	2020-08-26T13:06:08Z
dc.date.available	2020-08-26T13:06:08Z
dc.date.issued	1968
dc.identifier.uri	https://hdl.handle.net/11250/2674898
dc.description.abstract	The 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.iso	eng
dc.relation.ispartofseries	NGU (255)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	KARTLEGGING
dc.subject	FOLDNING
dc.subject	PETROGRAFI
dc.subject	SEDIMENTÆR BERGART
dc.subject	STRUKTURGEOLOGI
dc.subject	STØRKNINGSBERGART
dc.title	The geology of the Løkken area, Sør-Trøndelag.
dc.type	Journal article
dc.description.localcode	34947
dc.source.pagenumber	21-36 + ka

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