Show simple item record

dc.contributor.authorSolli, Arne
dc.contributor.authorTucker, Robert D.
dc.contributor.authorRobinson, Peter
dc.date.accessioned2020-07-15T08:18:22Z
dc.date.available2020-07-15T08:18:22Z
dc.date.issued1997
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2665768
dc.description.abstractThe report is a guidebook for a one day excursion in connection to the COPENA meeting held at NGU 18-22 August 1997. The excursion route is Trondheim- Orkanger-Lensvik-Agdenes-The report is a guidebook for a one day excursion in connection to the COPENA meeting held at NGU 18-22 August 1997. The excursion route is Trondheim- Orkanger-Lensvik-Agdenes-Ørlandet-Hasselvika-Rissa-Rørvik-Trondheim. The purpose of the excursions is to demonstrate lithologies in the Proterozoic basement in the Western Gneiss Region and the Caledonian nappe sequences that are down folded into the basement in thight synclines. The effect of the Scandian deformation and metamorphic overprinting on the Proterozoic gneisses will also be emphasised. The following tectonic units will be studied: Protero- zoic gneisses of the Western Gneiss Region; The Risberget Nappe consisting of augen gneisses; The Sætra Nappe consisting of flagstones; the Blåhø Nappe with mica schist, hornblende schist, amphibolite and marble; The lowgrade Støren Nappe with greenstones, schists, marbles and gabbroic to felsic intrusions: Devonian sediments.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (97.133)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRATIGRAFI
dc.subjectPREKAMBRIUM
dc.subjectDATERING
dc.subjectSTRUKTURGEOLOGI
dc.titleProterozoic Basement and Scandian Geology of the Outer Trondheimsfjord Region
dc.typeReport
dc.description.localcode44714
dc.source.pagenumber21


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

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