Vis enkel innførsel

dc.contributor.authorSørensen, Henning
dc.coverage.spatial19283 Melfjorden
dc.coverage.spatial19282 Svartisen
dc.date.accessioned2020-08-26T12:44:54Z
dc.date.available2020-08-26T12:44:54Z
dc.date.issued1955
dc.identifier.urihttps://hdl.handle.net/11250/2674634
dc.description.abstractThis study is a continuation of the work carried out by S. Skjeseth and the writer in 1952. The present paper only deals with an extremely well-exposed surface 1 km square in front of the retreating Engenbræ glacier. This surface is built up of a series of para-sediments metamorphosed under amphibolite facies conditions. The main components are: amphibolites (often with diopside and garnet), sillimanite-mica schists, lime-silicate gneisses, skarn, and crystalline limestone. The folding is intense with narrow and deep folds. A mass of peridotite is situated in a banded series lying between an upper series of mica schists (granite) and a lower series of calcareous rocks. It is shown that the peridotite was emplaced in an early stage of the folding in a zone of strong deformation and that this mass has much disturbed the surroundings during sebsequent phases of folding because of its greater rigidity.
dc.language.isoeng
dc.relation.ispartofseriesNGU (191)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectSTØRKNINGSBERGART
dc.subjectOMDANNET BERGART
dc.subjectMINERALOGI
dc.subjectOMDANNING
dc.subjectFOLDNING
dc.titleA petrographical and structural study of the rocks around the Peridotite at Engenbræ, Holandsfjord, Northern Norway. Bjergartene omkring peridotiten ved Engenbræen, Holandsfjord.
dc.typeJournal article
dc.description.localcode35562
dc.source.pagenumber71-102


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

  • Artikler [1064]
    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

Vis enkel innførsel

Navngivelse 4.0 Internasjonal
Med mindre annet er angitt, så er denne innførselen lisensiert som Navngivelse 4.0 Internasjonal