Gawler Craton - Western Eyre Peninsula, Coulta Subdomain and Nuyts Subdomain

Western Eyre Peninsula, Coulta Subdomain and Nuyts Subdomain

On western Eyre Peninsula, the Coulta Subdomain merges with the Nuyts Subdomain which is dominated by variably deformed ca. 1670-1610 Ma granitoids, mafics and felsic volcanics. Deformation is attributed to the Kalaran Orogeny which generated a major fold belt or shear zone, the Fowler Shear Zone, ca. 1600-1540 Ma.

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