The research area is located in the central part of North Macedonia, in the area of the Klepa Mts. Based on sedimentological, micropaleontological and biostratigraphical investigations of samples from both the east and west side of the Klepa Mts., se . . .

Oceanic obduction and ophiolite emplacement are processes which result in positioning of more dense oceanic lithosphere on top of less dense continental crust. It is known that obduction is related to the closure of oceanic realms, however exact mech . . .

In the central part of North Macedonia, in the area of the Klepa Mts., Upper Cretaceous sedimentary formations have been studied. Based on sedimentological, micropaleontological and biostratigraphical investigations of samples from both the east and . . .

The ophiolites of the Balkan Peninsula are distinguished into the Western and the Eastern Vardar ophiolites and it is generally accepted that both of them resulted from the latest Jurassic/earliest Cretaceous closure of the Vardar branch of the Tethy . . .

The Central Balkan region offers particular insights into the very last episodes of the life of oceanic domains that existed between Adria and Europe. This special issue highlights some of the latest developments in the geological research of this c . . .

U-Pb geochronology of zircon grains retrieved from magmatic rocks intruding the Jadar block terrane in the central Balkans is used here to add new constraints on the terrane accretion processes and the provenance of crustal sources of this potentiall . . .

The complex geodynamic evolution of the northernmost Neotethys is the subject of a long-living controversy. The most perplexing issues are related to the waning stage(s) of the Tethyan ocean(s) in the Balkans and the timing of the Europe-Adria collis . . .

Magnesium (Mg) and zinc (Zn) isotopes have been applied to trace whether surface carbonates have been recycled into the deep mantle beneath Balkan Peninsula, where a stagnant slab exists in the mantle transition zone. Here we investigate a suite of C . . .

The Sava Vardar Zone (Pamić, 2002) or the Sava Zone (Schmid et al., 2008) is a discontinued belt of Late Cretaceous to Palaeogene variably metamorphosed flysch-like deposits associated with roughly contemporaneous magmatic rocks, varying in composi . . .