Late Variscan orogenic collapse caused subsidence and forming extensional and transtensional basins of Pennsylvanian to Permian age in Bohemian Massif. PhD thesis will be focused on understanding tectonic regime of the basins and later reactivations. Most of the basins underwent partial deformation in compressional or transpressional regime during Mesozoic and Cenozoic. Thesis will be focused on collecting field sedimentological and structural data and low temperature dating techniques (AFTA, zircon FTA) and construction of kinematic models for individual basins in various time intervals. Work will also incorporate reinterpretation of subsurface data (well logs, seismic sections) and airborne geophysical data.
Předběžná náplň práce v anglickém jazyce
Late Variscan orogenic collapse caused subsidence and forming extensional and transtensional basins of Pennsylvanian to Permian age in Bohemian Massif. PhD thesis will be focused on understanding tectonic regime of the basins and later reactivations. Most of the basins underwent partial deformation in compressional or transpressional regime during Mesozoic and Cenozoic. Thesis will be focused on collecting field sedimentological and structural data and low temperature dating techniques (AFTA, zircon FTA) and construction of kinematic models for individual basins in various time intervals. Work will also incorporate reinterpretation of subsurface data (well logs, seismic sections) and airborne geophysical data.
- zadáno vedoucím/školitelem