Edmundian orogeny

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.^[1]

References

^ Piechoka and co-authors (2018). "Neoproterozoic 40Ar/39Ar mica ages mark the termination of a billion years of intraplate reworking in the Capricorn Orogen, Western Australia". Precambrian Research. pp. 391–406.

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

[1] Piechoka and co-authors (2018). "Neoproterozoic 40Ar/39Ar mica ages mark the termination of a billion years of intraplate reworking in the Capricorn Orogen, Western Australia". Precambrian Research. pp. 391–406.

[1]

See also

References