Lithostratigraphy of the Palaeogene - Lower Neogene succession of the Danish North Sea

Poul Schiøler, Jan Andsbjerg, Ole R. Clausen, Gregers Dam, Karen Dybkjær, Lars Hamberg, Claus Heilmann-Clausen, Erik P. Johannessen, Lars E. Kristensen, Iain Prince, Jan A. Rasmussen

Research output: Book/ReportBookResearchpeer-review

93 Citations (Scopus)

Abstract

As a result of a lithological, sedimentological and biostratigraphic study of well sections from the Danish sector of the North Sea, including some recently drilled exploration wells on the Ringkøbing-Fyn High, the lithostratigraphic framework for the siliciclastic Palaeogene to Lower Neogene sediments of the Danish sector of the North Sea is revised. The sediment package from the top of the Chalk Group to the base of the Nordland Group is subdivided into seven formations containing eleven new members. The existing Våle, Lista, Sele, Fur, Balder, Horda and Lark Formations of previously published lithostratigraphic schemes are adequate for a subdivision of the Danish sector at formation level. Bor is a new sandstone member of the Våle Formation. The Lista Formation is subdivided into three new mudstone members: Vile, Ve and Bue, and three new sandstone members: Tyr, Idun and Rind. Kolga is a new sandstone member of the Sele Formation. Hefring is a new sandstone member of the Horda Formation. Freja and Dula are two new sandstone members of the Lark Formation. Danish reference sections are established for the formations, and the descriptions of their lithology, biostratigraphy, age and palaeoenvironmental setting are updated.

Original languageEnglish
PublisherDe Nationale Geologiske Undersøgelser for Danmark og Grønland
Number of pages77
ISBN (Print)978-87-7871-196-0
DOIs
Publication statusPublished - 29 Jun 2007

Publication series

SeriesGeological Survey of Denmark and Greenland Bulletin
Number12
ISSN1604-8156

Keywords

  • Biostratigraphy
  • Lithostratigraphy
  • Neogene
  • North Sea Basin
  • Palaeogene

Programme Area

  • Programme Area 3: Energy Resources

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