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Mineral water resources in the Czech part of the Vienna basin
Bošková, Lucia ; Datel, Josef (advisor) ; Hrkal, Zbyněk (referee)
The bachelor thesis characterizes the Vienna Basin region from a geological and hydrogeological perspective. The main focus is put on the occurrence of mineral water. It describes the basic types of waters that are located there. In a closer look, it describes important types of them, mainly those ones that have the largest occurrence in the region. In another aspect, it analyzes their current condition and use. It defines basic concepts of this issue and describes common or legislative requirements for the classification and description of mineral waters. It puts a closer look and describes main sites of mineral water springs, including local spa places, especially those ones that are currently active. It also briefly deals with localities, where mineral water abstraction or spa treatment took place in the past and which are currently no longer active. In the end, it describes these sites from a balneological point of view. Keywords Vienna basin, mineral waters, spa, balneology
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Mineral water resources in the Czech part of the Vienna basin
Bošková, Lucia ; Datel, Josef (advisor) ; Hrkal, Zbyněk (referee)
The bachelor thesis characterizes the Vienna Basin region from a geological and hydrogeological perspective. The main focus is put on the occurrence of mineral water. It describes the basic types of waters that are located there. In a closer look, it describes important types of them, mainly those ones that have the largest occurrence in the region. In another aspect, it analyzes their current condition and use. It defines basic concepts of this issue and describes common or legislative requirements for the classification and description of mineral waters. It puts a closer look and describes main sites of mineral water springs, including local spa places, especially those ones that are currently active. It also briefly deals with localities, where mineral water abstraction or spa treatment took place in the past and which are currently no longer active. In the end, it describes these sites from a balneological point of view. Keywords Vienna basin, mineral waters, spa, balneology
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3D seismic interpretation and model of the Schrattenberg fault system in the Valtice area
Hlaváčková, Šárka ; Fischer, Tomáš (advisor) ; Buchta, Štěpán (referee)
3D SEISMIC INTERPRETATION AND MODEL OF THE SCHRATTENBERG FAULT SYSTEM IN THE VALTICE AREA Šárka Hlaváčková Abstract The Schrattenberg normal fault system represents a dominant feature of the western margin of the Vienna Basin. Along with the Steinberg fault, they controlled the sedimentary and tectonic development of the area, and considerably participated in the deposition of the basin fill during a relatively short period of time in the Miocene. A detailed interpretation of the fault system is essential for full understanding of the local basin development and its geological architecture. The oil exploration industry targets mainly the Steinberg and Schrattenberg fault system because of the occurrences of oil and natural gas deposits that are related to the basin tectonics, which forms structural traps sealed by the main fault systems or by minor synthetic or antithetic faults. The thesis presents a geological framework of the Mistelbach block near Valtice at the western margin of the Vienna Basin. Geological interpretation includes also the fault framework modeling with the emphasis on the course of the Schrattenberg fault system. The model was built in the Petrel interpretation software with the use of the principles of the 3D seismic interpretation. In particular, seismic stratigraphy methods, Petrel...
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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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