Jump to content

Kararan orogeny

Add links
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by OAbot (talk | contribs) at 04:21, 17 April 2020 (Open access bot: doi added to citation with #oabot.). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

The Kararan orogeny was an orogenic event in the Gawler Craton of Western Australia during the Proterozoic between 1.57 and 1.55 billion years ago which reworked rocks metamorphosed during the Kimban orogeny. [1][2]

See also

References

  1. ^ Payne, J.L. and co-authors (2007). "Temporal constraints on the timing of high-grade metamorphism in the northern Gawler Craton: implications for assembly of the Australian Proterozoic". Australian Journal of Earth Sciences: 623. doi:10.1080/08120090801982595. {{cite journal}}: Cite journal requires |journal= (help)
  2. ^ Myers, John S.; Shaw, Russell D.; Tyler, Ian M. (1996). "Tectonic evolution of Proterozoic Australia". Tectonics. 15 (6): 1431–1446. doi:10.1029/96TC02356.
Stub icon

This article about a specific Australian geological feature is a stub. You can help Wikipedia by expanding it.

Retrieved from "https://en.wikipedia.org/w/index.php?title=Kararan_orogeny&oldid=951435022"