dl | Geološki anali Balkanskoga poluostrva

Middle Jurassic radiolarian assemblages from Zlatar Mt. (SW Serbia)

Đerić, Nevenka (2010)

(middle Jurassic, radiolarians, Internal Dinarides, Komarani Village, SW Serbia)

Internal Dinarides); 4, Jadar and Kopaonik blocks (partof the Internal Dinarides); 5, Dinaridic and Western Vardar ophiolites (parallelizedwith the Mirdita ophiolites of Albania, obducted onto the internal Dinarides inJurassic

SIMIĆ120Fig. 1. Tectonic sketch of the Dinarides (after SCHMID et al. 2008), indicating theposition of the studied locality. The units mapped are, from external to internal:1, External Dinarides (without subdivisions); 2, East

DIMITRIJEVIĆ M.D. 2001. Dinarides and the Vardar Zone: ashort review of the geology. Acta Vulcanologica, 13: 1–8.DIMITRIJEVIĆ, M.D. & DIMITRIJEVIĆ, M.N. 1973. Olistostrome Mélange in the Yugoslavian Dinarides and LateMesozoic Plate

Chert blocks in the ophiolitic mélange of Zlatibor Mt. (SW Serbia) - age and geodynamic implications

Gerzina, Nataša (2016)

Cherts are quite frequently occurring rocks in the Internal Dinarides, an extremely complex area composed of several tectonostratigraphic units in which oceanic sediments, ophiolites and partly metamorphosed parts of the distal continental margin of Adria are preserved. Therefore, these cherts differ in age and the original depositional environment in which they were formed. Results of investigations carried out in the chert blocks found in the mélange in the vicinity of Jasenovo village on SE slopes of Zlatibor Mt. are ...

(cherts, radiolarians, ophiolitic mélange, Jurassic, Internal Dinarides, SW Serbia)

so-far in the Internal Dinarides ofSerbia reveal the following age clusters: Middle toLate Triassic, Middle Jurassic and Late Cretaceous.Early Jurassic ages have not been proven in the Internal Dinarides in Serbia, while Upper

the Internal Dinarides: a preliminary study based on selected regions. 5th International Symposium on Eastern Mediterranean Geology, Thessaloniki, Greece, 14. –20. April2004.DIMITRIJEVIĆ, M. D., 2001: Dinarides and the Vardar

Triassic and Jurassic radiolarians occur inchert blocks embedded in mélange of Late Jurassicage in the Internal Dinarides (e.g. OBRADOVIĆ et al.1987/88; GORIČAN et al. 1999; VISHNEVSKAYA et al.2009; OZSVÁRT & KOVÁCS 2012; GAWLICK

The Rhynchonellide brachiopod Cyclothyris ? globata (Arnaud, 1877) from the Santonian-Campanian of Pannonides, Carpatho-Balkanides and Dinarides (southeastern Europe)

Radulović, Vladan (2002)

(rhynchonellide brachiopod, Cyclothyris ? globata, Cretaceous, Santonian-Campanian, stratigraphy, Pannonides, Carpatho-Balkanides, Dinarides)

Correlation of metabasic rocks from metamorphic soles of the Dinaridic and the Western Vardar Zone ophiolites (Serbia): three contrasting pressure-temperature-time paths

Srećković-Batoćanin, Danica (2012)

(Serbia, Western Vardar Zone, Dinarides, ophiolites, metamorphic sole, metabasic rocks, amphibole, PT conditions, correlation)

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. Постојећи теренски

beneath the Brezovicaharzburgite Massif. In: KARAMATA, S. & JANKOVIĆ, S.(eds.), Geology and Metallogeny of the Dinarides andthe Vardar zone. Proceedings of the International Symposium. Academy of Science & Arts of the Republic

with the Banjskaultramafic massif. In: KARAMATA, S. & JANKOVIĆ, S.(eds.), Geology and Metallogeny of the Dinarides andthe Vardar zone. Proceedings of the International Symposium Academy of Science & Arts of the Republic ofSrpska

The role of the 'Zvornik suture' for assessing the number of Neotethyan oceans: Surface - subsurface constraints on the fossil plate margin (Vardar Zone vs. Inner Dinarides)

Spahić Darko ()

The balancing exercise of the “single-ocean model” and reexa - mination of Jurassic paleogeographic conditions and tectonic interaction allowed the reconstruction of the mosaic of independent microplate margins and sutured northwestern Tethyan realm (Vardar Ocean). The overprinted Mesozoic convergent margin referred to as the ‘Zvornik suture’ was of special interest in the reconstruction of the displaced ophiolite belts of Dinarides and Vardar Zone. The surface–subsurface constraints of these mixed crustal units, in particular the polyphase strike-slip character of the ...

('Zvornik suture’ Inner Dinarides,, West Vardar Zone, Vardar Zone s.s., 'Dinaric Tethys', subsurface crustal faults.)

unitscoined the name Dinarides: Dinarides s.s., hellenidesand Taurides. Modern-day Dinarides are referringto the Dinarides s.s. (the focus of this study is theeastern domain of the Dinarides s.s.). Dinarides s.s.as a southern

geotectonic subdivision of Dinarides isdivision in the Inner- (or Internal, e.g., hrVATOVIć &PAMIć, 2005) and the External Dinarides (e.g., rOyDeN,1988; PAMIć, 1998, 2002; DIMITrIJeVIć, 1997, 1999).Dinarides are comprised of the

from Jurassic SSZ type-ophiolites formedalong the entire length of the Dinarides towardsAlbania, and Greece (>1200 km). The sub con -tinental Inner Dinarides to depleted mid-oceanridge/arc compositions have often been document