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It is characterized by deep-water sedimentary rocks of Triassic,Jurassic, Cretaceous and Paleogene age, developed inseveral thrust units. Cretaceous-Paleogene flysch formation represents the youngest formation within theBudva

Paleodictyon latum VIALOV & GOLEV have been identified from the Cretaceous-Paleogene flysch of the Budva Zone. Nereites irregularisIchnofossils from Cretaceous-Paleogene flysch of Mide locality(Budva Zone, southern Montene

Montenegro)MARTIN ĐAKOVIĆ1, GORAN ĆULAFIĆ2, MILEVA MILIĆ1,DAMJAN ČAĐENOVIĆ1 & NOVO RADULOVIĆ1Abstract. Cretaceous-Paleogene flysch represents the youngest formation in the Budva Zone. Although theMaastrichtian-Lower Eocene age of

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(upper Cretaceous magmatic suite, volcanism, volcanic facies, sediments)
QUADT etal. 2002, 2004, 2005; CLARK & ULLRICH 2004;Upper Cretaceous magmatic suites of the Timok Magmatic ComplexMIODRAG BANJEŠEVIĆ1Abstract. The Upper Cretaceous Timok Magmatic Complex (TMC) developed on a continental crust

features of the Srednogorie Zone (Bulgaria), an Upper Cretaceous Intra-arc Basin. SedimentaryGeology, 19: 39–68.ANTONIJEVIĆ, I., GRUBIĆ, A. & ĐORĐEVIĆ, M. 1974. TheUpper Cretaceous paleorift in eastern Serbia. In: KARAMATA, S. (ed

korice - naslov.qxpIntroductionThe Upper Cretaceous volcanо-sedimentary complex of the Carpatho–Balkanides belt spreads discontinuously from the northern parts of the ApuseniMountains and Banat in Romania, over Timok Krajina

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(subsurface geology, blocks subsidence, Upper Cretaceous, Miocene, Quaternary, Belgrade)
route of thenew bridge. Upper Cretaceous–Paleogene flysch deposits represent the oldest unit, which make the basement rock for the overlying Miocene and Quaternarysediments.Upper Cretaceous – PaleogeneThe basement rocks of

on the presence ofnannoplankton species, the Upper Cretaceous age wasconfirmed. According to ANĐELKOVIĆ (1987), the flysch was formed at the end of the Upper Cretaceous andEarly Paleogene.The Ostružnica flysch strata were

cascade subsided along sub-parallel faults towards N–NW.Key words: Subsurface geology, blocks subsidence, Upper Cretaceous, Miocene, Quaternary, Belgrade.Апстракт. Највећи мост на свету са једним носећим пилоном отворен је у Београду

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initiation of the late Early Cretaceous nappe-stacking in the ductile to semi-ductile/semi-brittle domain.Key words: structural analysis, flat-ramp geometry, Supragetic Unit, late Early Cretaceous thrustingАпстракт. Набори везани

late Early to early Late Cretaceous, post‘Austrian’, cooling event which was reported in Serbo-Macedonian Massif (ANTIĆ et al., 2016) was interpreted as post-collisional extension. The Late Cretaceous Banatitic magmatism in

Ceahlau-Severin and theDanubian Units took place after the cessation of theLate Cretaceous Banatitic magmatism, during the latest Cretaceous-Early Paleocene (BOJAR et al., 1998;IANCU et al., 2005a; SCHMID et al., 2008; ANTIĆ

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(marine macroinvertebrates, diversity, biotic crisis, OAE2, Eastern Caucasus, Cenomanian/Turonioan, Late Cretaceous)
black organic-rich laminated marlstonesLate Cretaceous marine biodiversity dynamics in the Eastern Caucasus, northern Neo-Tethys Ocean 35Fig. 4. Dynamics of the Late Cretaceous global (afterPURDY 2008) and regional (Azerbaijan

Background and Plans for Research. In:GINSBURG, R.N. & BEAUDOIN, B. (eds.), Cretaceous Resources, Events, and Rhythms. NATO ASI Series, SeriesLate Cretaceous marine biodiversity dynamics in the Eastern Caucasus, northern Neo-Tethys

HOFMANN, P. & WAGNER, T. (2008). Isotopic Evidencefor Glaciation During the Cretaceous Supergreenhouse.Science, 319: 189–192.CARON, M. 1985. Cretaceous planktic foraminifera. In:BOLLI, H.M., SAUNDERS, J.B. & PERCH-NIELSEN, K

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(dasycladales, new taxon, bio-erosion, diagenesis, Upper Cretaceous, Santonian, SW Serbia, Mirdita Zone)
skeleton. Salpingoporella nicolacarrasispec. nov. was found in the Novi Pazar area, in an outcrop of Late Cretaceous limestones belonging to theNW Rogozna–Novi Pazar–S Golija Mt. belt (in shortNovi Pazar belt, Mirdita Zone

belt, also called the western belt of theVardar Zone, i.e. Dinarides by some authors. In thisarea, the Late Cretaceous succession transgressivelyrests on the Paleozoic, showing a transition from shallow-water to basinal environments

bio-erosion, described under the name of Mur1.Key words: Dasycladales, new taxon, bio-erosion, diagenesis, Upper Cretaceous, Santonian, SW Serbia,Mirdita Zone.Абстракт. Нова врста Salpingoporrlla nicolacarrasi описана је из сантонских

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(brachiopods, gastropods, taxonomic diversity, transgression, Early Cretaceous, Lesser Caucasus, Azerbaijan, Neo-Tethys Ocean)
tectonic processes inthe Early Cretaceous, including hot-spot activity(AZIZBEKOV et al. 1972; ISMAIL-ZADEH 2007; ADAMIAet al. 2011; ROLLAND et al. 2009, 2011).The regional Lower Cretaceous stratigraphy hasbeen developed,

methodsThis study employs regional and global stratigraphical ranges of Early Cretaceous brachiopods and gasTaxonomic diversity dynamics of Early Cretaceous brachiopods and gastropods in the Azerbaijanian domains 19Fig. 2. The

taxonomic review of Cretaceous brachiopodsfrom Azerbaijan, which remains essential source ofthe relevant information up to nowadays. These dataare the result of regional sampling of many Early Cretaceous fossil localities in