Classes
- Dynamic Earth: outstanding issues of modern geology +1MBCPLUS023 | Faculty of Science
- Research Project in Geology and PaleontologyMG420E01 | Faculty of Science
- Plutons, volcanoes, and orogeny through timeMG420P10 | 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
- Timing, styles, and kinematics of Cambro-Ordovician extension in the Teplá-Barrandian Unit, Bohemian Massif, and its bearing on the opening of the Rheic Ocean2013 | Faculty of Science
- Neoproterozoic to early Cambrian Franciscan-type mélanges in the Teplá-Barrandian unit, Bohemian Massif: Evidence of modern-style accretionary processes along the Cadomian active margin of Gondwana?2013 | Faculty of Science
- From Cadomian accretion to Variscan collision: a crustal-scale traverse across the northwestern Teplá–Barrandian unit2013 | Faculty of Science
- Deciphering the Variscan tectonothermal overprint and deformation partitioning in the Cadomian basement of the Teplá-Barrandian unit, Bohemian Massif2012 | Faculty of Science
- Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif2012 | Faculty of Science
- Structure and stratigraphy of the Tepla-Barrandian Neoproterozoic, Bohemian Massif: A new plate-tectonic reinterpretation2011 | Faculty of Science
- Structure, emplacement, and tectonic setting of Late Devonian granitoid plutons in the Tepla-Barrandian unit, Bohemian Massif2011 | Faculty of Science
- Subduction-driven shortening and differential exhumation in a Cadomian accretionary wedge: The Teplá-Barrandian unit, Bohemian Massif2010 | 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
- Hot plutonism in a cold accretionary wedge: What terminated the Cadomian orogeny along the northern periphery of Gondwana?2023 | Faculty of Science
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