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Abstract Cambrian deposition along eastern Gondwana extends from the western Koonenberry and Loch Lilly–Kars belts to the eastern Saint Arnaud and Warrata groups (and other covered Thomson Orogen units). Farther east, the Lachlan Orogen’s Ordovician depositional system comprises turbidite packages of the Adaminaby, Castlemaine and Girilambone groups.
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