Collected Item: “Tectonic evolution of the Vršac Mts. (NE Serbia): Inferences from field kinematic and microstructural investigations”
Врста публикације
Рад у часопису
Верзија рада
објављена верзија
Језик рада
енглески
Аутор/и (Милан Марковић, Никола Николић)
Uroš Stojadinović, Nemanja Krstekanić, Bojan Kostić, Marija Ružić, Aleksa Luković
Наслов рада (Наслов - поднаслов)
Tectonic evolution of the Vršac Mts. (NE Serbia): Inferences from field kinematic and microstructural investigations
Наслов часописа
Geologica Carpathica
Издавач (Београд : Просвета)
Central Library of the Slovak Academy of Sciences
Година издавања
2021
Сажетак на енглеском језику
The Vršac Mts. in NE Serbia represent the key area to investigate structural relations between the Northern
Serbo-Macedonian Subunit and Supragetic Unit of the Dacia Mega-Unit. The geodynamic events during the Variscan
orogeny in the Late Paleozoic colligated the two units and led to their metamorphic differentiation. The Late Cretaceous
extension exhumed the medium-grade Serbo-Macedonian metamorphic rocks and structurally juxtaposed them against
the low-grade metamorphosed basement of the Supragetic Unit along an E-dipping shear zone, which outcrops in
the crystalline basement of the Vršac Mts. The subsequent Oligocene–Miocene extension, which led to the formation of
the Pannonian Basin, overprinted the effects of earlier tectonic phases to a large extent. Hence, large segments of
the Northern Serbo-Macedonian Subunit and the Supragetic Unit, including their contact, were buried beneath
the Neogene deposits of the southern part of Pannonian Basin. The tectonic uplift of the Vršac Mts. occurred in middle to
late Miocene times along the SW-dipping normal faults that controlled deposition in the adjacent Zagajica Depression.
The Miocene extension, triggered by the retreat of Carpathian slab, exhumed the crystalline basement of the mountains,
and exposed the Late Cretaceous Serbo-Macedonian/Supragetic extensional contact.
Serbo-Macedonian Subunit and Supragetic Unit of the Dacia Mega-Unit. The geodynamic events during the Variscan
orogeny in the Late Paleozoic colligated the two units and led to their metamorphic differentiation. The Late Cretaceous
extension exhumed the medium-grade Serbo-Macedonian metamorphic rocks and structurally juxtaposed them against
the low-grade metamorphosed basement of the Supragetic Unit along an E-dipping shear zone, which outcrops in
the crystalline basement of the Vršac Mts. The subsequent Oligocene–Miocene extension, which led to the formation of
the Pannonian Basin, overprinted the effects of earlier tectonic phases to a large extent. Hence, large segments of
the Northern Serbo-Macedonian Subunit and the Supragetic Unit, including their contact, were buried beneath
the Neogene deposits of the southern part of Pannonian Basin. The tectonic uplift of the Vršac Mts. occurred in middle to
late Miocene times along the SW-dipping normal faults that controlled deposition in the adjacent Zagajica Depression.
The Miocene extension, triggered by the retreat of Carpathian slab, exhumed the crystalline basement of the mountains,
and exposed the Late Cretaceous Serbo-Macedonian/Supragetic extensional contact.
Број часописа
5
Почетна страна
395
Завршна страна
405
DOI број
https://doi.org/10.31577/GeolCarp.72.5.3
ISSN број часописа
1335-0552
Кључне речи на српском (одвојене знаком ", ")
severna srpsko-makedonska subjedinica, supragetikum, kinematska analiza, multifazna ekstenzionalna deformacija
Кључне речи на енглеском (одвојене знаком ", ")
Northern Serbo-Macedonian Subunit, Supragetic Unit, kinematic analysis, multi-stage extensional deformations.
Шира категорија рада према правилнику МПНТ
M20
Ужа категорија рада према правилнику МПНТ
М23
Степен доступности
Отворени приступ
Лиценца
Creative Commons – Attribution-Share Alike 4.0 International
Формат дигиталног објекта
.pdf