Miltalie orogeny

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

References
  1. Payne, J.L. and co-authors (2009). "Evolution of the Mawson Continent". The Geological Society of London. pp. 322–324.


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