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dc.contributor.authorRoberts, David
dc.contributor.authorSundvoll, Bjørn
dc.coverage.spatial16204 Budal
dc.description.abstractTrondhjemite dykes forming part of a swarm cutting the Gula Group metasedimentsand tectonically overlying Støren Group metabasalts in the district south ofStøren, Sør-Trøndelag, have been investigated in road-cuts in the Snøan area.Geochemically, the fine-grained dykes are high-Al2O3 trondhjemites which showclear trace and rare-earth elements signatures indicative of a continentalmargin setting. An attempt at Rb-Sr radiometric dating produced a best-fitisochron of 465 +- Ma, interpreted as a minimum age for the dyke swarm. Thedyke has also probably been affected by thermal resetting.The dykes do not penetrate the Lower Hovin Group succession which unconformablyoverlies the Støren Group volcanites, and contains fossils of Late Arenig age.The Rb-Sr minimum age is thus in reasonable accord with the faunal evidence.The trondhjemite dyke swarm was evidently emplacement into a thickened conti-nental margin crust following obduction of the Støren ocean-floor basalts uponthe Gula, with coeval deformation, metamorphism and subsequent uplift, probablyin earliest Ordovician time.
dc.relation.ispartofseriesNGU-Rapport (96.163)
dc.rightsNavngivelse 4.0 Internasjonal
dc.titleGeochemistry and Rb-Sr dating of trondhjemite dykes from the Gula Group, near Snøan, Sør-Trøndelag.

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