Rayner orogeny
 | This article needs additional citations for verification. (November 2019) |
The Rayner orogeny was a mountain building that thickened the early continental crust (the cratonic nucleus) of what is now East Antarctica 3.5 billion years ago. Rocks preserving the orogeny are found in the rough vicinity of the Scott Mountains between Enderby Land in the north and Kemp Land in the south.[1]
See also
[edit]References
[edit]- ^ Anderson, John B. (1999). "Antarctic Marine Geology". Cambridge University Press. p. 31-32. ISBN 9780521593175.
 | This orogeny article is a stub. You can help Wikipedia by expanding it. |