dc.contributor.author | Graversen, Ole | |
dc.coverage.spatial | 19143 Ski | |
dc.date.accessioned | 2020-08-26T13:11:34Z | |
dc.date.available | 2020-08-26T13:11:34Z | |
dc.date.issued | 1973 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674970 | |
dc.description.abstract | Garnet amphibolite bands folded together with gneiss lamellae in tight to isoclina folds are described. A structural analysis shows that the folds were formed during two separate deformation episodes. This conclusion has in particular a bearing on the problem of distinguishing between primary intrusive structures and simple and multiple fold-structures. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU (300) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | PREKAMBRIUM | |
dc.subject | OMDANNET BERGART | |
dc.subject | PETROGRAFI | |
dc.subject | FOLDNING | |
dc.subject | PERM | |
dc.subject | STRUKTURGEOLOGI | |
dc.title | Structural interpretation of a double-folded gneiss-amphibolite sequence, Bunnefjorden, Akershus. | |
dc.type | Journal article | |
dc.description.localcode | 36308 | |
dc.source.pagenumber | 73-82 + k | |