Duško Vujačić
Goran Barović
Đurđica Perović
GEOLOŠKE KARAKTERISTIKE POLIMLJA, REGION CRNA GORA I
SRBIJA
DOI: 10.35666/28310438.2020.5.131
UDC: 911.2:55(497.16+497.11Polimlje)
Abstract: Tectonics and geologic material were processed based on maps and interpreters for the Basic Geological Map 1: 100 000: "Gusinje" (Mirković et al, 1968), "Ivangrad", "Bijelo Polje" (Živaljević et al., 1981, 1983), "Prijepolje" (Ćirić et al., 1978), "Pljevlja" and "Višegrad", as well as a review of the literature related to this issue. The investigated area belongs to the Durmitor Unit of the Dinarides (Karamata et al., 1997), and only the northernmost part, the lowest corners of the studied area around the Potpeć reservoir; belong to the Ofiol131131ytic Zone (Karamata et al., 1997). The Durmitor unit covers the north of Montenegro and the far southwest of Serbia and generally extends into the middle of the Dinarides. A series of branch forms for cores of Paleozoic rocks extend from the Paleozoic Lima formations to the mid-Bosnian shale mountains (Marovic, 2001). The southwestern border of the Durmitor Zone is known as the "Durmitor Cover". This structure, with its numerous tectonic windows, half-windows, and tectonic pistons, shows that it was at least decakilometrically transported to the southwest via the upper Cretaceous flysch zone of the Vis Krš, located within the Dalmatian-Herzegovina unit (Karamata et al., 1997). On the northeastern side, it is underlain by the Ophiolite Belt (Karamata et al., 1997), which is marked by the entire length of this contact between the diabase-corneal formation and the shale shales (the Ophiolite Belt) and the Triassic, Lias and Dodger limestones of the Durmitor Unit (Marovic, 2001).
Key words: paleozoic, tectonic, zone, Polimlje, Lim River, Montenegro, Serbia