Loch Ness Supergroup
Loch Ness Supergroup | |
---|---|
Stratigraphic range: 1000–720 Ma | |
Type | Geological supergroup |
Sub-units | Loch Eil Group, Glenfinnan Group, Badenoch Group |
Underlies | Dalradian Supergroup |
Overlies | Wester Ross Supergroup with tectonic contact |
Area | Northwestern Scotland |
Thickness | 6–9 km |
Lithology | |
Primary | Semi-pelite, Pelite, Psammite |
Other | Quartzite |
Type section | |
Named for | Loch Ness |
The Loch Ness Supergroup is one of the subdivisions of the Neoproterozoic sequence of sedimentary rocks (or their metamorphic equivalents) in the Scottish Highlands.[1] It is found everywhere in tectonic contact above the older Wester Ross Supergroup. It is thought to be unconformable overlain by the Cryogenian to Cambrian Dalradian Supergroup.[2]
References[edit]
- ^ British Geological Survey. "Loch Ness Supergroup". BGS Lexicon of named rock units. Retrieved 31 May 2024.
- ^ Krabbendam, M.; Strachan, R.; Prave, T. (2022). "A new stratigraphic framework for the early Neoproterozoic successions of Scotland". Journal of the Geological Society. 179. doi:10.1144/jgs2021-05.