Classes
- Plutons, volcanoes, and orogeny through timeMG420P10 | Faculty of Science
- Dynamic Earth: outstanding issues of modern geology +1MBCPLUS023 | Faculty of Science
- Research Project in Geology and PaleontologyMG420E01 | Faculty of Science
- Field course of geologyMG420T06 | Faculty of Science
- Physical geology IMG421P00 | Faculty of Science
- Physical geology I (for teachers)MG421P00U | Faculty of Science
- Brittle tectonicsMG421P30 | Faculty of Science
- Introduction to Physical Geology +1MG421P31 | Faculty of Science
- Magmatic systemsMG421P37 | Faculty of Science
- Geologic field trips +1MG421T04 | Faculty of Science
Publications
- Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif2012 | Faculty of Science
- Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif2009 | Faculty of Science
- Four magmatic fabrics in the Tuolumne batholith, central Sierra Nevada, California (USA): Implications for interpreting fabric patterns in plutons and evolution of magma chambers in the upper crust2007 | Faculty of Science
- Tectonic evolution of a continental magmatic arc from transpression in the upper crust to exhumation of mid-crustal orogenic root recorded by episodically emplaced plutons: the Central Bohemian Plutonic Complex (Bohemian Massif)2005 | Faculty of Science
- Multiple Fabric Patterns and Emplacement Mechanisms of a Composite Batolith: A Result of Polyphase Tectonic Evolution of Continental Magmatic Arc (Central Bohemian Batolith, Bohemian Massif)2003 | First Faculty of Medicine, Faculty of Mathematics and Physics
- Multiple Fabric Patterns and Emplacement Mechanisms of a Composite Batolith: A Result of Polyphase Tectonic Evolution of Continental Magmatic Arc (Central Bohemian Batolith, Bohemian Massif)2003 | Faculty of Science
- Hot plutonism in a cold accretionary wedge: What terminated the Cadomian orogeny along the northern periphery of Gondwana?2023 | Faculty of Science
- Dynamics of Cambro-Ordovician rifting of the northern margin of Gondwana as revealed by the timing of subsidence and magmatism in rift-related basins2023 | Faculty of Science
- Analysis of fracturing processes leading to caldera collapse2023 | Faculty of Science
- Multi-stage metal enrichment and formation of gold mineralization in black shales: the role of high heat flow in a rift setting2023 | Faculty of Science
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