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dc.contributor.authorSturt, Brian A.
dc.contributor.authorSundvoll, Bjørn
dc.contributor.authorAskvik, Helge
dc.coverage.spatial13212 Kristiansund
dc.date.accessioned2020-08-26T09:02:18Z
dc.date.available2020-08-26T09:02:18Z
dc.date.issued1997
dc.identifier.urihttps://hdl.handle.net/11250/2674093
dc.description.abstractA Rb-Sr whole-rock isochron from a quartz-syenite dyke at Stabben, Nordmøre, has provided an age of 263 +- 6Ma. This could be taken to indicate a crystallisation age for the dyke, i.e. Early Permian. The age, however, does not conform with an earlier published age for a similar dyke on the nearby island of Tustna, or with a published Middle\/Late Carboniferous palaeomagnetic pole for the Stabben dyke. It may be that the isochron is dating hydrothermal alteration of the dyke. The presence of such dykes with a deep mantle magmatic source, along the Møre-Trøndelag Fault Zone, emphasies the fundamental nature of the fault and indicates that a period of tensional conditions pertained during the time of emplacement of the dykes.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (432)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGANGBERGART
dc.subjectGANGBERGART
dc.subjectOMVANDLING
dc.titleA probable Permian hydrothermal alteration age for a quartz syenite dyke from Stabben, Nordmøre.
dc.typeJournal article
dc.description.localcode49120
dc.source.pagenumber71-75


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