Earth:Balder Formation
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Balder Formation Stratigraphic range: Earliest Eocene ~55–52 Ma | |
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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.[1] 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.[2]
References
- ↑ British Geological Survey. "Balder Formation". http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=BALD.
- ↑ Morton A.C.; Knox R.W.O'B. "Geochemistry of late Palaeocene and early Eocene tephras from the North Sea Basin". Journal of the Geological Society, London 147 (3): 425–437. doi:10.1144/gsjgs.147.3.0425. http://jgs.lyellcollection.org/content/jgs/147/3/425.full.pdf.
Original source: https://en.wikipedia.org/wiki/Balder Formation.
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