Deformation in the Gangåsvann area.
dc.contributor.author | Peacey, J. Springer | |
dc.coverage.spatial | 15214 Snillfjord | |
dc.coverage.spatial | 15213 Løkken | |
dc.coverage.spatial | 15212 Hølonda | |
dc.coverage.spatial | 15211 Orkanger | |
dc.coverage.spatial | HITRA | |
dc.coverage.spatial | HEIM | |
dc.coverage.spatial | ORKLAND | |
dc.date.accessioned | 2020-08-26T12:54:24Z | |
dc.date.available | 2020-08-26T12:54:24Z | |
dc.date.issued | 1963 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674768 | |
dc.description.abstract | The effects of multiple deformation on a series of banded metasedimentary rocks is described. Disharmonic folding has occurred and a slide formed during the first phase of movement separates highly folded rocks from those above which are less deformed. The isoclinal recumbent folds of the first phase have been re-folded across steeply dipping axial planes to give a characteristic pattern of acurate outcrops. ater movements have produced open folds and rejuvenation of the slide. The development of faults and a fracture system is the final phase of deformation. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU (223) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | STRUKTURGEOLOGI | |
dc.subject | PETROGRAFI | |
dc.subject | FOLDNING | |
dc.subject | OMDANNET BERGART | |
dc.title | Deformation in the Gangåsvann area. | |
dc.type | Journal article | |
dc.description.localcode | 35349 | |
dc.source.pagenumber | 275-293 |
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