Balder Formation | |
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Stratigraphic range: Earliest Eocene ~55–52 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓ | |
Type | Formation |
Unit of | Moray Group |
Underlies | Horda, Mousa or Tay Formation |
Overlies | Sele or Dornoch Formation, Montrose Group |
Thickness | 30–300 m (98–984 ft) |
Lithology | |
Primary | Mudstone, tuff |
Other | Sandstone |
Location | |
Region | Offshore; subsurface |
Country | United Kingdom Norway Denmark |
Extent | Central and northern North Sea, Faroe-Shetland Basin |
Type section | |
Named for | Balder, Norse deity |
The Balder Formation is a geological formation of lowermost Eocene in age, found in the Central and Northern North Sea and Faroe-Shetland Basin. The formation is named after Balder, a god from Norse mythology. Layers of tuff are found, particularly at the base of the unit, deposited by airfall from volcanoes associated with the North Atlantic Igneous Province.
References
- British Geological Survey. "Balder Formation". The BGS Lexicon of Named Rock Units.
- Morton A.C.; Knox R.W.O'B (1990). "Geochemistry of late Palaeocene and early Eocene tephras from the North Sea Basin" (PDF). Journal of the Geological Society, London. 147 (3): 425–437. Bibcode:1990JGSoc.147..425M. doi:10.1144/gsjgs.147.3.0425.