Geology of Kosovo
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Geologic History, Stratigraphy & Tectonics
- Kacanik Flysch
- 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.
- Brezovica harzburgite
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- Moores, E.M.; Fairbridge, Rhodes W. 1997, p. 309-310.
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