Vrska Cuka granite: An example of Carpatho-Balkan units. Early Paleozoic granites followed by a gap in the Aptian and pelagic clastic rocks from the Cretaceous.
Novo Brdo area: Part of the Central Vardar zone. Situated south of a highly tectonized domain. Novo Brdo schist formed in the Triassic in a volcano-sedimentary basin.
