According to the tectonic architecture of the Balkan Peninsula, the territory of Macedonia belongs to the Dinarides, Rhodope and Carpatho-Balkanides. In a relatively small area, Macedonia has a very complex geological and tectonic structure, which was shaped by intense and long-term processes, followed by magmatism of a wide spectrum, from the ultrabasic to the acidic. From a stratigraphic point of view, geological formations consist of the oldest Precambrian high-grade metamorphic rocks to the youngest Quaternary deposits, and such a ...
Hristina Petrova, Uroš Stojadinović, Boris Vakanjac, Vesna Ristić Vakanjac, Katarzyna Wątor, Piotr Rusiniak, Ewa Kmiecik. "Link between active tectonics/faulting and mineral and thermal water occurrence in Republic of North Macedonia" in Review of the Bulgarian Geological Society, Bulgarian Geological Society (2024). https://doi.org/10.52215/rev.bgs.2024.85.3.221
