Early Paleozoic Cenerian (Sardic) geodynamic relationships of peripheral eastern north Gondwana affinities : revisiting the Ordovician of the Getic/Kučaj nappe (eastern Serbia)

Spahić, Darko; Tančić, Pavle; Barjaktarović, Dejan

doi:10.7306/gq.1675

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Tytuł artykułu

Early Paleozoic Cenerian (Sardic) geodynamic relationships of peripheral eastern north Gondwana affinities : revisiting the Ordovician of the Getic/Kučaj nappe (eastern Serbia)

Autorzy

Spahić Darko , Tančić Pavle , Barjaktarović Dejan

Treść / Zawartość

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Identyfikatory

DOI

10.7306/gq.1675

Warianty tytułu

Języki publikacji

Abstrakty

Regional tectonic synthesis suggests that a segment of the bipartite eastern Gondwana-type Carpathian-Balkan nappe-stacked Getic/Kučaj/Supragetic basement (eastern Serbia) experienced Cambro-Ordovician Cenerian (Sardic) accretionary-type deformation. The Ordovician basement of the Alpine Getic/Kučaj nappe exposes an earlier-mapped shallow-marine transgressive-type Fe-silicate-rich ironstone sequence. The Ordovician ironstone is used as second-order evidence of a hitherto untraceable tectonically-driven unconformity. Early Paleozoic compression is consistent with the controversial latest Cambrian to intra-Ordovician Cenerian (Sardic) interval, documented by (i) a 488 Ma metamorphic event and available detrital zircon data (Serbo-Macedonian gneissic unit), (ii) a deformed Lower Ordovician Getic/Kučaj brachiopod assembly, and (iii) an intra-Ordovician unconformity dividing the Supragetic basement/”Vlasina complex”. The data further imply that mafic gabbro-dominating sills, cropping out in the northern Getic/Kučaj unit, are consistent with Ordovician back-arc activity. The Getic/Kučaj gabbro is Ordovician in age, piercing a Neoproterozoic–Cambrian (Lower Ordovician) Supragetic/”Vlasina complex”, overlain by a transgressive Silurian–Devonian sedimentary sequence. The emergence of Ordovician mafic intrusions reflects submarine volcanism, while deep-water redox conditions were capable of a sustained supply of Fe (similar to Sardinia). In terms of tectono-palaeogeographic reconstructions, the origin of Ordovician shortening and mafic volcanism is often challenged. The latter is broadly analogous with the embryonic eastern Rheic Ocean, corresponding additionally to the Armorican spur and related intra-continental magmatism.

Słowa kluczowe

eastern north Gondwana Ordovician ironstones Cenerian (Sardic) event glacio-eustatic changes eastern Serbia

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2023

Tom

Vol. 67, No. 1

Strony

art. no. 5

Opis fizyczny

Bibliogr. 149 poz., map., rys., wykr.

Twórcy

autor

Spahić Darko

darkogeo2002@hotmail.com

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

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

autor

Tančić Pavle

University of Belgrade, Institute of Chemistry, Technology and Metallurgy, Department for Catalysis and Chemical Engineering-National Institute of the Republic of Serbia, Njegoševa 12, 11000 Belgrade, Serbia

https://orcid.org/0000-0002-4024-710X

autor

Barjaktarović Dejan

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

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