Miltalie orogeny
 | This article needs additional citations for verification. (November 2019) |
The Miltalie orogeny also termed the Miltalie event was a small orogenic event 400 millions after the Sleaford orogeny in the Proterozoic, indicated by metasedimentary rocks preserved in the Miltalie Gneiss.[1]
See also
[edit]References
[edit]- ^ Payne, J.L. and co-authors (2009). "Evolution of the Mawson Continent". The Geological Society of London. pp. 322–324.
-crop.jpg){kind=small} | This article about a specific Australian geological feature is a stub. You can help Wikipedia by expanding it. |