Vis enkel innførsel

dc.contributor.authorLaughton, A.S.
dc.date.accessioned2020-08-26T13:14:43Z
dc.date.available2020-08-26T13:14:43Z
dc.date.issued1975
dc.identifier.urihttps://hdl.handle.net/11250/2675014
dc.description.abstractThe hypotheses of sea floor spreading and plate tectonics enable the evolution of ocean basins to be understood provided that there are adequate data on the present and past plate boundaries from the magnetic anomaly patterns and some geological control of the nature of age of critical parts of the ocean floor. From such data, the following main phases of evolution of the north-east Atlantic from a Triassic unrifted continental mass have been identified: 1. Early Jurassic (80 my). 2. Early Cretaceous (120 my). 3. Late Cretaceous (80 my). 4. Palaeocene (60 my) 5. Middle Eocene (45 my). 6. Middle Oligocene (30 my). 7. Miocene (15 my). 8. Present (0 my).
dc.language.isoeng
dc.relation.ispartofseriesNGU (316)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectTEKTONIKK
dc.subjectSTRATIGRAFI
dc.titleTectonic evolution of the Northeast Atlantic ocean: a review.
dc.typeJournal article
dc.description.localcode35900
dc.source.pagenumber169-193


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