Nataša Gerzina Spajić

University of Belgrade

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Nevenka Djerić

University of Belgrade

N. Yu. Bragin

Geological Institute

NĐ

Nevenka Đerić

University of Belgrade

ЛГ

Л. Г. Брагина

Geological Institute

Szilvia Kövér

HUN-REN Institute of Earth Physics and Space Science

László Fodor

Eötvös Loránd University

L. F. Kopayevich

Lomonosov Moscow State University

Gábor Héja

Mining and Geological Survey of Hungary

ЛФ

Л. Ф. Копаевич

Lomonosov Moscow State University

Liubov Bragina

Geological Institute

Cooperative Institutions

Eötvös Loránd University

Institute for Geological and Geochemical Research

Hungarian Academy of Sciences

Pázmány Péter Catholic University

Geological Institute

University of Belgrade

Mining and Geological Survey of Hungary

Russian Academy of Sciences

HUN-REN Institute of Earth Physics and Space Science

Hungarian Research Network

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Stratigraphy and microfossils (radiolarians and planktonic foraminifers) of the Upper Cretaceous (upper Santonian–lower Campanian) Struganik limestone (Western Serbia)

Palaeoworld (2019)

Л. Г. Брагина N. Yu. Bragin L. F. Kopayevich Nevenka Djerić Nataša Gerzina Spajić

Calcarenite

Carbonate platform

10.1016/j.palwor.2019.05.001

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Citations (4)

New radiolarian data from the Jurassic ophiolitic mélange of Avala Mountain (Serbia, Belgrade Region)

Swiss Journal of Geosciences (2018)

N. Yu. Bragin Liubov Bragina Nataša Gerzina Spajić Nevenka Djerić Stefan M. Schmid

Ladinian

Obduction

Radiolaria

10.1007/s00015-018-0313-8

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Citations (8)

New paleomagnetic results from the Inner Dinarides, SW Serbia

Emő Márton László Fodor Szilvia Kövér Vesna Lesić Nevenka Đerić

As a result of the paleomagnetic co-operation between Hungarian and Serbian specialists in the last decades a paleomagnetic paper was published about the Fruska Gora (Lesic et al., 2007) and an other one about the magnetic fabrics of the intrusive and extrusive magmatic rocks of the Kopaonik area (Lesic et al., 2013). During more recent years several overstep sequences were tested from the Western Vardar zone. The aim of our present study was to find out if the units belonging to the Inner Dinarides rotated in the same sense as the overstep sequences or different rotations occurred. For that reason we sampled 12 localities within the research area. Five of which represent Late Cretaceous sediments in the area of Tara Mt., while the others geographically distributed Triassic and Jurassic succession. The sampled localities belong to different thrust sheets.

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Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides

Swiss Journal of Geosciences (2018)

Kristóf Porkoláb Szilvia Kövér Zsolt Benkó Gábor Héja Melinda Fialowski

We have investigated successive episodes of ocean-continent and continent–continent convergence in Western Serbia (Drina-Ivanjica thrust sheet). The coupled application of structural and petrological analyses with Illite Crystallinity measurements and K/Ar dating has revealed the timing and structural characteristics of multiple regional deformation phases, and allowed us to revise the origin of the different Triassic units outcropping in the study area. D1 tectonic burial was characterized by anchizonal metamorphism, dominantly WNW-verging isoclinal folding (F1), and related axial planar cleavage (S1) formation in the Paleozoic basement and the stratigraphic cover of the Drina-Ivanjica thrust sheet exposed along the northern rim of this thrust sheet. The timing of D1 deformation is constrained by K/Ar ages suggesting 135–150 Ma tectonic burial for the Drina-Ivanjica thrust sheet. D1 deformation and metamorphism is correlated with the closure of the Vardar ocean by top-W to NW ophiolite obduction and the underthrusting of the Adriatic distal passive margin below the oceanic upper plate. Since D1 structures are lacking in the southern occurrences of Triassic rocks within the study area it is proposed that this Triassic is may not be the original sedimentary cover of the Drina-Ivanjica Paleozoic basement. We propose that this southern Triassic originated from a more external Dinaridic thrust sheet and was transported to its present-day position by a top-NE backthrust presumably during late Early Cretaceous–Paleogene times. Map-scale, NW–SE striking D2 thrust faults and abundant NW–SE trending F2 folds observed in all units correspond to the general trend of the Dinaridic orogen and are attributed to the latest Cretaceous–Paleogene collision between Adria and Europe. Regional Latest Cretaceous–Paleogene shortening was followed by strike-slip tectonics (N–S shortening and perpendicular extension) and subsequent Miocene normal faulting in both orogen-parallel and orogen-perpendicular directions driven by slab rollback processes of the Carpathian-Dinaridic realm.

Obduction

Paleogene

Thrust fault

Basement

10.1007/s00015-018-0327-2

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Citations (32)

Stratigraphy and Microfauna (Radiolarians and Foraminifera) of the Upper Cretaceous (Upper Santonian–Lower Campanian) Carbonate Deposits in the Area of Struganik Village, Western Serbia)

Stratigraphy and Geological Correlation (2020)

Л. Г. Брагина N. Yu. Bragin Л. Ф. Копаевич Nevenka Djerić Nataša Gerzina Spajić

Carbonate platform

Microfauna

10.1134/s0869593820010037

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Citations (3)