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A rift-related mafic dyke swarm in the Corrovarre Nappe of the Caledonian Middle Allochthon, Troms, North Norway, and its tectonometamorphic evolution

dc.contributor.authorZwaan, Bouke K.
dc.contributor.authorvan Roermund, Herman L. M.
dc.date.accessioned2020-08-26T09:12:38Z
dc.date.available2020-08-26T09:12:38Z
dc.date.issued1990
dc.identifier.urihttps://hdl.handle.net/11250/2674273
dc.description.abstractForkortet. The Corrovarre Nappe is the highest tectonic unit of the Kalak Nappe Complex, in the Caledonian Allochthon, in the Nordreisa area of Troms, North Norway. The nappe consists of meta-arkoses, metapellites and calc-silicate schists intruded by gabbroic sills and associated mafic dykes.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (419)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRATIGRAFI
dc.subjectOMDANNING
dc.subjectTEKTONIKK
dc.subjectPETROGRAFI
dc.subjectGANGBERGART
dc.subjectPALEOZOIKUM
dc.subjectGEOKRONOLOGI
dc.titleA rift-related mafic dyke swarm in the Corrovarre Nappe of the Caledonian Middle Allochthon, Troms, North Norway, and its tectonometamorphic evolution
dc.typeJournal article
dc.description.localcode35299
dc.source.pagenumber25-44


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