Edmundian orogeny

{{Use Australian English|date=May 2024}}

{{Use dmy dates|date=April 2022}}

{{more citations needed|date=November 2019}}

The Edmundian orogeny is a preserved low-grade reworking of sedimentary to metasedimentary rocks in the Gascoyne Complex of Western Australia from 1.68 billion to 1.46 billion years ago.{{cite news|title=Neoproterozoic 40Ar/39Ar mica ages mark the termination of a billion years of intraplate reworking in the Capricorn Orogen, Western Australia |year=2018|publisher=Precambrian Research |url= https://www.sciencedirect.com/science/article/pii/S0301926818300019|author=Piechoka and co-authors |pages=391–406}}