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The geological evolution of the Vienna basin and interpretation of seismic profiles across the western margin of the basin
Hlaváčková, Šárka ; Fischer, Tomáš (advisor) ; Berka, Jiří (referee)
The geological evolution of the Vienna basin and interpretation of seismic profiles across the western margin of the basin Abstract The Vienna basin represents an example of a Neogene pull-apart basin developed between two orogenic systems - the Eastern Alps and West Carpathians. Their different Miocene geodynamic played the key role in opening of the basin. The pull-apart mechanism was significantly influenced by a rotation in the Middle Miocene. This thesis summarize the geodynamic development of the basin with regard to Tertiary evolution of the wider Carpathian - Panonnian area and paleomagnetic description of a rotation of ALCAPA unit. The Lower Miocene basin is superimposed on stack of nappes of the Alpine - Carpathian thrust belt. It was formed as a piggy-back basin on the top of overthrusted nappes. During the Karpathian, a new tectonic settings was established, due to the change of geodynamics within the Alpine - Carpathian area. In the Badenian, the important NE - SW trending faults were developed. The Steinberg and Schrattenberg synsedimentary faults considerably participated in the formation of the west margin of the Vienna basin, and controlled a deposition of the Neogene sedimentary fill, reaching a maximum thickness of 5500 m. In my undergraduate thesis, I target the local development of the...

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