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dc.contributor.authorFossen, Haakon
dc.contributor.authorNissen, August L.
dc.coverage.spatial19233 Blåfjellhatten
dc.date.accessioned2020-08-26T09:07:39Z
dc.date.available2020-08-26T09:07:39Z
dc.date.issued1990
dc.identifier.urihttps://hdl.handle.net/11250/2674194
dc.description.abstractRb-Sr isotope whole-rock dating of undeformed and unaltered parts of the Blåfjellhatten granite has yielded an isochron age of 1356 +- 29 Ma with I.R.=0.7254 +-0.0027, interpreted as the age of intrusion. This age contrasts with an earlier interpretation of the granite as part of the 1780-1650 Ma Transscandinavian Granite-Porphyry Belt and with other dates from the Grong-Olden Culmination and other basement windows in the central Norwegian Caledonides. The new data indicate that the Blåfjellhatten granite is not directly related to any of the major tectonothermal events of the Baltic Shield.
dc.language.isonor
dc.relation.ispartofseriesNGU Bulletin (420)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectDATERING
dc.subjectGRANITT
dc.subjectKALEDONSKE FJELLKJEDE
dc.titleRb-Sr age of the Blåfjellhatten granite in the Olden Window, Central Norway.
dc.typeJournal article
dc.description.localcode36267
dc.source.pagenumber51-56


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