International Geological Journal - Official Journal of the Carpathian-Balkan Geological Association

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Exhumation history of the Juhor Mts. in Central Serbia, the Northern Serbo–Macedonian Subunit

Published: Jun 2024

Pages: 213 - 223

DOI: https://doi.org/10.31577/GeolCarp.2024.12

Authors: UROS STOJADINOVIC, HAN NAH POMELLA, NEMANJA KRSTEKANIĆ, BOJAN KOSTIĆ, MAJA MALEŠ, NIKOLA RANDJELOVIC, MILOŠ RADONJIĆ

Abstract: In this study, we combined low-t thermochronology with outcrop- to micro-scale kinematic and petrological observations in the metamorphic basement of the Juhor Mts. in Central Serbia. The Juhor Mts. comprise northern parts of the Europe-derived Serbo–Macedonian Unit, at the transition towards the Adria-derived tectonic units of the Internal Dinarides. The Late Paleozoic Variscan orogeny resulted in the medium-grade greenschist to amphibolite facies metamorphism in the core of the mountains, as inferred from our thin section-scale observations. During the subsequent Alpine orogeny, the tectonic setting of the entire Europe–Adria transitional area was strongly influenced by the geodynamic evolution of the intervening Neotethyan Vardar Ocean. The last recorded thermal overprint in the northern segments of the Serbo–Macedonian metamorphics occurred in the latest Jurassic due to their burial during the obduction of the Eastern Vardar ophiolites over the European continental margin. According to our thermochronological and field structural data, the exhumation of the Juhor Mts. metamorphic basement occurred during two separate phases of extensional deformations. During the Late Cretaceous extension, the Serbo–Macedonian metamorphics were exhumed for ~3 to 6 km along a ductile Morava shear zone, and later structurally juxtaposed against the low-grade metamorphics of the adjacent Supragetic Unit of the Serbian Carpathians. The latest phase of ~1 to 2,5 km tectonic exhumation and uplift in the Miocene took place along the brittle normal faults that accommodated the opening of the Morava Valley Corridor, which forms the southern prolongation of the Pannonian Basin. It is plausible, therefore, that these Miocene normal faults are reactivated segments of thrusts inherited from the preceding Paleogene phase of the Adria–Europe collision.

Keywords: Northern Serbo–Macedonian Subunit, low-t thermochronology, kinematic analyses, extensional deformations

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