dc.contributor.author | Møller, Charlotte | |
dc.coverage.spatial | TRØNDELAG | |
dc.coverage.spatial | MØRE OG ROMSDAL | |
dc.date.accessioned | 2020-08-26T09:06:24Z | |
dc.date.available | 2020-08-26T09:06:24Z | |
dc.date.issued | 1988 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674176 | |
dc.description.abstract | Forkortet.In the gneiss area of northern Vestranden, kilometre-scale upright domes andbasins refold tight and isoclinal folds of banded amphibolite facies ortho-gneisses and supracrustal rocks. In the Roan area, a major culmination and itscore exposes a window, the Roan Igneous Complex (RIC). | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU Bulletin (413) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | GABBRO | |
dc.subject | OMDANNING | |
dc.subject | KALEDONSKE FJELLKJEDE | |
dc.subject | STRUKTURGEOLOGI | |
dc.title | Geology and metamorphic evolution of the Roan area, Vestranden, Western Gneiss Region, Central Norwegian Caledonides. | |
dc.type | Journal article | |
dc.description.localcode | 35140 | |
dc.source.pagenumber | 1-31 | |