Late Ruker orogeny

This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Find sources: "Late Ruker orogeny" – news · newspapers · books · scholar · JSTOR (November 2019) (Learn how and when to remove this template message)

The Late Ruker orogeny, also known as the Nimrod orogeny, was a

Red beds were deposited and are now preserved in the Ritscher Upland of Queen Maud Land. Stromatolite carbonate beds and quartz arenite in the Shackleton Range serves as evidence for a stable platform and epicratonic sea during the period.^[1]

See also

• List of orogenies
• Geology of Antarctica

References

This orogeny article is a stub. You can help Wikipedia by expanding it.

• v
• t
• e