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depleted mid-oceanridge/arc compositions have often been document -ed within the Vardar Zone (fig. 1c).Configuration of the Vardar Zone s.s.The Vardar Zone s.s. (coined by kOSSMAT 1924) isa composite Neotethyan suture comprised of

(identified by the Inner Dinaric Ophiolite Belt) and the Vardar Ocean(identified by the West Vardar Zone). The West Vardar Zone remains to be asubzone of the principal composite Neotethyan suture referred to as theVardar

protracted strike-slipactivity of the ‘Zvornik suture’.Key words:‘Zvornik suture’, Inner Dinarides,West Vardar Zone, Vardar Zone s.s.,‘Dinaric Tethys’, subsurface crustalfaults. Апстракт. Евалуација досадашњих резултата из домена

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(dimension stone, Vardar Zone, Tertiary granitoids, southern Serbia)
ofexploration methods of Tertiary magmatic complexesin the Vardar Zone of Serbia (Fig. 1) at the level ofreconnaissance survey. The Tertiary volcanic complexes of the Vardar zone have proved to be morecompliable for use as crushed

northern and westernSerbian part of the Vardar Zone (Cer, Boranja, Kosmaj, Brajkovac, Bukulja) are presented in KUREŠEVIĆ(2013b).The formation of Tertiary magmatic complexes ofthe Vardar Zone is connected with geotectonic evolution

rectangular frame) in the Vardar Zone (tectonic units according toKARAMATA, 2006 and ROBERTSON et al., 2009); CBES, Carpato-Balcanides of Eastern Serbia; SMU, Serbian-Macedonian Unit; MVZ, Main Vardar Zone; KBRU, Kopaonik Blockand

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(ostracodes, latest Permian (Changhsingian), taxonomy, stratigraphy, Vardar Zone, Jadar Block, NW Serbia)
Bosnia (Fig. 1A).This tectonostratigraphic unit is today an exoticblock terrane within the Vardar Zone. It is surroundedby the Vardar Zone Western Belt, except on the farthest south-eastern part where it is in direct contactwith

(KARAMATA et al. 2000; KARAMATA 2006): SMU – Serbian-Macedonian Unit;MVZ – Main Vardar Zone; KBRU – Kopaonik Block and Ridge Unit; VZWB – Vardar Zone Western Belt; JB – Jadar Block; DIE – Drina–Ivanjica Element; DOB –Dinaridic

from the Jadar Block (Vardar Zone, NW Serbia) 25Fig. 2. Distribution of conodonts and ostracodes in the Permian–Triassic boundary interval in theKomirićSection in NWSerbia, Jadar Block, Vardar Zone (modified after SUDARet

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(Serbia, Western Vardar Zone, Dinarides, ophiolites, metamorphic sole, metabasic rocks, amphibole, PT conditions, correlation)
korice - naslov.qxpCorrelation of metabasic rocks from metamorphic soles of theDinaridic and the Western Vardar zone ophiolites (Serbia):three contrasting pressure-temperature-time pathsDANICA SREĆKOVIĆ-BATOĆANIN1, NADA VASKOVIĆ1

sole rocks recorded beneath the Fruška Gora, Povlen (Tejići), Stolovi and Banjska ophiolites in theWestern Vardar Zone (WVZ) and beneath the Zlatibor, Bistrica, Sjenički Ozren and Brezovica ophiolites inthe Dinaridic ophiolite

as an important key in geodynamic evolution of the Mesozoic Tethyan ophiolites.Key words: Serbia, Western Vardar Zone, Dinarides, ophiolites, metamorphic sole, metabasic rocks,amphibole, PT conditions, correlation.Апстракт

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(brahiopods, Cyclothyris ? globata, Terebratula sp. (gen. et sp. nov.), foraminifera, stratigraphy, Lowermost Campanian, Guča, Vardar Zone, western Serbia)
are the questions answered in thecontroversial text “Senonian of the Vardar Zone”, asfollows (translation from Serbian): “Senonian rocks inthe Vardar Zone are represented by a particular Diabase-Chert Formation. They form a

was found in the Upper Cretaceoussuccession at the Dupljaj Stream, near Guča, in theBjelica Belt of the Vardar Zone (western Serbia) (Fig.1). The occurrences in ex-Yugoslavia of Cyclothyris?globata, which is common in several

were described and dated as Campanian by RADULOVIĆ & MOTCHUROVA-DEKOVA (2002). In several localities of the Vardar Zone (Guča, western Serbia) andthe Balkans (the Shumen Formation, northern Bulgaria), C.? globata was found in