Jump to content

Miltalie orogeny

From Wikipedia, the free encyclopedia

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