Vestiges of Cambro-Ordovician continental accretion in the Carpathian-Balkan orogen: First evidence of the ‘Cenerian’ event in the central Serbo-Macedonian Unit

Spahić, Darko; Bojić, Zoran; Popović, Danica; Gaudenyi, Tivadar

doi:10.24425/agp.2020.134558

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Tytuł artykułu

Vestiges of Cambro-Ordovician continental accretion in the Carpathian-Balkan orogen: First evidence of the ‘Cenerian’ event in the central Serbo-Macedonian Unit

Autorzy

Spahić Darko , Bojić Zoran , Popović Danica , Gaudenyi Tivadar

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Identyfikatory

DOI

10.24425/agp.2020.134558

Warianty tytułu

Języki publikacji

Abstrakty

In the Balkans, the Serbo-Macedonian Unit (SMU), Serbia, is thrust bounded by the composite Tethyan Vardar Zone and the Carpatho-Balkanides. The SMU actually emerges from beneath the Neoalpine Miocene-Pliocene deposits. Both provenance and geodynamic position of the SMU are poorly known and still debated. This paper reviews the data hitherto published and includes some new field data interpretations. The SMU is composed of a Neoproterozoic-Cambrian high-grade (para- and ortho-) gneiss with peraluminous magmatic arc components (560-470 Ma). The SMU is in the contact with Neoproterozoic upper Ordovician-Carboniferous low-grade metasedimentary succession of an accretionary wedge assembly represented by the Supragetic basement. The SMU basement became folded, sheared and metamorphosed around 490-450 Ma. Paleomagnetic data point to high southern latitudes and a peri-Gondwanan position of the SMU at that time, which concurs with glaciomarine evidence recorded from the upper Ordovician sediments at the base of an accretionary wedge succession. Based on the published data and field survey in the Stalać region, we correlate the SMU with the pre-Mesozoic gneiss terrane exposed in the Strona-Ceneri zone of the Alps. This terrane, identified as the Cenerian orogen of the Alaskan subduction type, developed at an active margin of Gondwana during middle Ordovician times. The SMU basement, with augen and migmatitic gneisses and arc-related peraluminous magmatic bodies, developed at this margin as part of the Cenerian belt or its equivalent. Such an orogenic edifice proved transient and in the earliest Silurian the SMU fragments drifted away being bound for Baltica (amalgamated Moesian microplate and Danubian terrane) to which they became accreted in the Carboniferous and included in the southern European branch of the Variscan orogen (Marginal Dacides/Carpatho-Balkanides). Despite consider-able Variscan and Alpine reworking, the pre-Variscan, Cenerian-type crustal assembly along with an inferred boundary between the magmatic arc and the accretionary wedge, accompanied by back-arc/forearc deposits, are still decipherable in the Western Balkan countries.

Słowa kluczowe

Cenerian event North Gondwana Serbo-Macedonian Unit supragetic basement Lower Paleozoic paleosuture migmatites shear zones

Gondwana dolny paleozoik migmatyt strefa ścinania

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2021

Tom

Vol. 71, no. 2

Strony

219--247

Opis fizyczny

Bibliogr. 148 poz., rys., tab.

Twórcy

autor

Spahić Darko

darko.spahic@gzs.gov.rs

Geological Survey of Serbia, Rovinjska 12, 11000 Belgrade, Serbia

https://orcid.org/0000-0002-5832-0782

autor

Bojić Zoran

Geological Survey of Serbia, Rovinjska 12, 11000 Belgrade, Serbia

autor

Popović Danica

Geological Survey of Serbia, Rovinjska 12, 11000 Belgrade, Serbia

autor

Gaudenyi Tivadar

Geographical Institute “Jovan Cvijić” of the Serbian Academy of Sciences and Arts, Djure Jakšića 9, 11000 Belgrade, Serbia.

https://orcid.org/0000-0002-1843-2384+++

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Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2021).

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