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Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations. The pavements show banded Dalgaringa gneiss cut by several generations of granite and pegmatite veins, possibly of Wooramel and Moorarie age. West at the top. S 178-82; Lstr 253-32

Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations. The pavements show banded Dalgaringa gneiss cut by several generations of granite and pegmatite veins, possibly of Wooramel and Moorarie age. West at the top. S 178-82; Lstr 253-32

Photograph: Cees Passchier