Vis enkel innførsel

dc.contributor.authorZiegler, Peter A.
dc.date.accessioned2020-08-26T13:14:06Z
dc.date.available2020-08-26T13:14:06Z
dc.date.issued1975
dc.identifier.urihttps://hdl.handle.net/11250/2674997
dc.description.abstractThe development history of the North Sea area can be subdivided into five stages: 1) Caledonian geosynclinal stage (Cambrian-Silurian), 2) Variscan geosynclinal stage (Devoanin-Carboniferous), 3) Permo-Triassic intracratonic stage, 4) Jurassic-Cretaceous taphrogenic rifting stage, 5) Tertiary post-rifting intracratonic stage. The Jurassic-Cretaceous North Sea central rift system is related to the rifting processes in the Arctic North Atlantic. During the Tertiary this sector of the Atlantic entered the drifting stage. At the same time the North Sea rift system became inactive, leading to regional subsidence. Emplacement of the late Tertiary Rh\u00F4ne-Rhine rift system postdates the central North Sea rift.
dc.language.isoeng
dc.relation.ispartofseriesNGU (316)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRATIGRAFI
dc.subjectBERGGRUNNSGEOLOGI
dc.subjectTEKTONIKK
dc.titleThe geological evolution of the North Sea area in the tectonic framework of North Western Europe.
dc.typeJournal article
dc.description.localcode35888
dc.source.pagenumber1-27


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