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 gneiss rafts in younger less deformed granite pegmatite veins. North at the top
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 gneiss rafts in younger less deformed granite pegmatite veins. North at the top
Photograph: Cees Passchier