Edmundian orogeny explained

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]

See also

Notes and References

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

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