Browse Items (6 total)

Global population is growing rapidly. As a result, increasingly large areas are being settled and farmed. This devastates soils and causes pollution by heavy metals and other components. Heavy metals in the environment originate from both natural and…
Alzarog Taher Mohamed,Vakanjac Boris,Jelić Ivana,Ristić Vakanjac Vesna,Naunović Zorana,Gajić Vuk,Đorđević-Milošević Suzana.

Cretaceous-Paleogene flysch represents the youngest formation in the Budva Zone. Although the Maastrichtian-Lower Eocene age of these rocks has been well documented in the literature, trace fossils are only mentioned as abundant and not described. In…
Đaković Martin,Ćulafić Goran,Milić Mileva,Čađenović Damjan,Radulović Novo.

Berane Basin in Montenegro has been known for rich paleoflora of diverse geological ages. The remains of paleovegetation of various ages were preserved by the lake occurring in this area from Late Oligocene to Early Pliocene. Therefore, the shifts in…
Đorđević-Milutinović Desa,Stevanović Branka,Ćulafić Goran.

Elephantoid cheek teeth from the late Early and Middle Miocene of Europe frequently display mixtures of bunodont and zygodont features, making their taxonomical attributions difficult and subjective. Today, these teeth with “intermediate”…
Radović Predrag,Bradić-Milinović Katarina.

This paper addresses a Drina-Ivanjica basement member, Drina Formation, characterized by ŕ controversial Neoproterozoic to Carboniferous age. The Drina Formation is also informally referred to as the “Lower Drina Formation” and the “Upper Drina…
Spahić Darko,Glavaš-Trbić Bojan,Đajić Slavica,Gaudenyi Tivadar.

Lece magmatic complex in SE Serbia, part of the Serbo-Macedonian Metallogenic Province, is one of the most promising zones for lead, zinc and precious metals for the country. This complex was formed as a result of the post-collisional magmatic…
Velojić Miloš,Prelević Dejan,Jelenković Rade.
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