dc.contributor.author | Zwaan, Bouke K. | |
dc.contributor.author | van Roermund, Herman L. M. | |
dc.date.accessioned | 2020-08-26T09:12:38Z | |
dc.date.available | 2020-08-26T09:12:38Z | |
dc.date.issued | 1990 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674273 | |
dc.description.abstract | Forkortet. 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.iso | eng | |
dc.relation.ispartofseries | NGU Bulletin (419) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | STRATIGRAFI | |
dc.subject | OMDANNING | |
dc.subject | TEKTONIKK | |
dc.subject | PETROGRAFI | |
dc.subject | GANGBERGART | |
dc.subject | PALEOZOIKUM | |
dc.subject | GEOKRONOLOGI | |
dc.title | A rift-related mafic dyke swarm in the Corrovarre Nappe of the Caledonian Middle Allochthon, Troms, North Norway, and its tectonometamorphic evolution | |
dc.type | Journal article | |
dc.description.localcode | 35299 | |
dc.source.pagenumber | 25-44 | |