Mesozoic – a secondary geological driver that lasted about 185 mln. Years (250-65 mln.) and is divided into TRIAs, Jarsky and a lifted period. In Macedonia, predominantly in the Western Macedonian and Vardar zone, and with smaller masses in the Serbian-Macedonian massif, with TRIA, JURIAN and urged rock complexes. Triass is widespread, above all in the Western Macedonian zone, and less in the Vardar zone, where it is composed of basal conglomerates, sandstones, clympic and limestone, with a maximum thickness of up to 650-700 m. The Jurassic period is dominantly developed in the Vardar zone and is presented with several remains of the former continuous and widespread ocean bark, built from the bottom level of gabs, basal, spilly-pylolaves and upper level of conglomerates, sandstones, clicples, mostly located between Demir Kapija-Gevgelija, at Skopska Crna Gora, on Klepa (Veles), etc. They are hacked with upper-jar granitoids. Volcanic-sedimentary rocks have been developed on the areas of Korab, Deshat and Jablanica. The regular period is developed with flaw and carbonate sediments in the Vardar zone with a thickness of up to 4,500 m, and with a small mass of sandstones, limestone and anhydrite in the tunal zone zone in Debar. N. Dum.
Original article in Macedonian language Cyrillic alphabet
Кириличен напис МЕЗОЗОИК