The Podolian Domain in southern Sarmantia is made mostly of Archaean - Palaeoproterozoic granulites ( up to 3.7 Ga ) .
The Podolian Domain in southern Sarmantia is divided by major faults into the Vinnitsa and Gayvoron regions .
The Podolian Domain in southern Sarmantia is made mostly of Archaean - Palaeoproterozoic granulites ( up to 3.7 Ga ) and divided by major faults into the Vinnitsa and Gayvoron regions .