Geology of Kosovo
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- 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. [2]
References
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- ↑ Moores, E.M.; Fairbridge, Rhodes W. (1997). Encyclopedia of European & Asian Regional Geology. Springer. pp. 309–310.
- ↑ Lafe, Emil, ed. (2009). Fjalor Enciklopedik Shqiptar [Encyclopedic Dictionary of Albania] (in Albanian). Vol. 2. Tirana: Academy of Sciences of Albania. p. 1294. ISBN 9789995610272. OCLC 426069353.
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