Quaternary tectonic and depositional evolution of eastern Srem (northwest Serbia)
The area of eastern Srem is situated in the southern periphery of the Pannonian basin. Its depositional evolution during the Neogene and the Quaternary has been controlled by tectonic processes. Miocene extensional subsidence was followed by the Pliocene-Quaternary inversion of the basin....
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| Format: | Article |
| Language: | English |
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Faculty of Mining and Geology, Belgrade
2014-01-01
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| Series: | Geološki Anali Balkanskoga Poluostrva |
| Subjects: | |
| Online Access: | http://www.doiserbia.nb.rs/img/doi/0350-0608/2014/0350-06081475043T.pdf |
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| author | Toljić Marinko Nenadić Draženko Stojadinović Uroš Gaudenyi Tivadar Bogićević Katarina |
| author_facet | Toljić Marinko Nenadić Draženko Stojadinović Uroš Gaudenyi Tivadar Bogićević Katarina |
| author_sort | Toljić Marinko |
| collection | DOAJ |
| description | The area of eastern Srem is situated in the southern periphery of the
Pannonian basin. Its depositional evolution during the Neogene and the
Quaternary has been controlled by tectonic processes. Miocene extensional
subsidence was followed by the Pliocene-Quaternary inversion of the basin.
The latter was accomplished as the result of replacement of the tensile by
the compressive stress field. Since the Late Neogene, the regional tectonic
activity has been controlled by compressive stress produced by the
northnortheastern propagation of the Adria microplate. In the compressive
NE-SW-oriented stress field, the recent structural plan of the Pannonian
basin and its wider environment, including its southern periphery, was
reactivated. The youngest tectonic deformations are characterized by positive
and negative vertical motions of large intrabasinal segments and basinal
periphery, resulting in the final inversion of the basin. The effects of the
basinal inversion can be recognized in genetic features of Quaternary
sediments and geomorphological characteristics of the relief. Sources of data
used for the interpretation of the Quaternary tectonic activity in the area
of eastern Srem are of geological, geomorphological, thermochronological, and
geophysical character. The positions of prominent fault structures have been
ascertained by remote sensing, interpretations of available geophysical
cross-sections, and using the field data. [Projekat Ministarstva nauke
Republike Srbije, br. 176015] |
| first_indexed | 2024-12-22T11:12:34Z |
| format | Article |
| id | doaj.art-f90f71ddc79e4f8f91004a5cd453fe92 |
| institution | Directory Open Access Journal |
| issn | 0350-0608 2406-0747 |
| language | English |
| last_indexed | 2024-12-22T11:12:34Z |
| publishDate | 2014-01-01 |
| publisher | Faculty of Mining and Geology, Belgrade |
| record_format | Article |
| series | Geološki Anali Balkanskoga Poluostrva |
| spelling | doaj.art-f90f71ddc79e4f8f91004a5cd453fe922022-12-21T18:28:08ZengFaculty of Mining and Geology, BelgradeGeološki Anali Balkanskoga Poluostrva0350-06082406-07472014-01-01201475435710.2298/GABP1475043T0350-06081475043TQuaternary tectonic and depositional evolution of eastern Srem (northwest Serbia)Toljić Marinko0Nenadić Draženko1Stojadinović Uroš2Gaudenyi Tivadar3Bogićević Katarina4Faculty of Mining and Geology, Department of Historical and Dynamic geology, BelgradeFaculty of Mining and Geology, Department of Historical and Dynamic geology, BelgradeFaculty of Mining and Geology, Department of Historical and Dynamic geology, Belgrade + Netherlands Research Centre for Integrated Solid Earth Science, VU University Amsterdam, Amsterdam, The NetherlandsGeographical Institute „Jovan Cvijić“, Serbian Academy od Sciences and Arts, BelgradeFaculty of Mining and Geology, Department of Historical and Dynamic geology, BelgradeThe area of eastern Srem is situated in the southern periphery of the Pannonian basin. Its depositional evolution during the Neogene and the Quaternary has been controlled by tectonic processes. Miocene extensional subsidence was followed by the Pliocene-Quaternary inversion of the basin. The latter was accomplished as the result of replacement of the tensile by the compressive stress field. Since the Late Neogene, the regional tectonic activity has been controlled by compressive stress produced by the northnortheastern propagation of the Adria microplate. In the compressive NE-SW-oriented stress field, the recent structural plan of the Pannonian basin and its wider environment, including its southern periphery, was reactivated. The youngest tectonic deformations are characterized by positive and negative vertical motions of large intrabasinal segments and basinal periphery, resulting in the final inversion of the basin. The effects of the basinal inversion can be recognized in genetic features of Quaternary sediments and geomorphological characteristics of the relief. Sources of data used for the interpretation of the Quaternary tectonic activity in the area of eastern Srem are of geological, geomorphological, thermochronological, and geophysical character. The positions of prominent fault structures have been ascertained by remote sensing, interpretations of available geophysical cross-sections, and using the field data. [Projekat Ministarstva nauke Republike Srbije, br. 176015]http://www.doiserbia.nb.rs/img/doi/0350-0608/2014/0350-06081475043T.pdftectonic activityPannonian basinnorthwest Serbiasubsidencebasin inversioneastern SremQuaternary |
| spellingShingle | Toljić Marinko Nenadić Draženko Stojadinović Uroš Gaudenyi Tivadar Bogićević Katarina Quaternary tectonic and depositional evolution of eastern Srem (northwest Serbia) Geološki Anali Balkanskoga Poluostrva tectonic activity Pannonian basin northwest Serbia subsidence basin inversion eastern Srem Quaternary |
| title | Quaternary tectonic and depositional evolution of eastern Srem (northwest Serbia) |
| title_full | Quaternary tectonic and depositional evolution of eastern Srem (northwest Serbia) |
| title_fullStr | Quaternary tectonic and depositional evolution of eastern Srem (northwest Serbia) |
| title_full_unstemmed | Quaternary tectonic and depositional evolution of eastern Srem (northwest Serbia) |
| title_short | Quaternary tectonic and depositional evolution of eastern Srem (northwest Serbia) |
| title_sort | quaternary tectonic and depositional evolution of eastern srem northwest serbia |
| topic | tectonic activity Pannonian basin northwest Serbia subsidence basin inversion eastern Srem Quaternary |
| url | http://www.doiserbia.nb.rs/img/doi/0350-0608/2014/0350-06081475043T.pdf |
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