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
- Multistage magma emplacement and progressive strain accumulation in the shallow-level Krkonoše-Jizera plutonic complex, Bohemian Massif2013 | Faculty of Science
- From Cadomian accretion to Variscan collision: a crustal-scale traverse across the northwestern Teplá–Barrandian unit2013 | Faculty of Science
- Magnetic fabric and tectonic setting of the Early to Middle Jurassic felsic dykes at Pitt Point and Mount Reece, eastern Graham Land, Antarctica2012 | Faculty of Science, Central Library of Charles University
- Formation and transfer of stoped blocks into magma chambers: The high-temperature interplay between focused porous flow, cracking, channel flow, host-rock anisotropy, and regional deformation2012 | Faculty of Science
- Structure, emplacement, and tectonic setting of Late Devonian granitoid plutons in the Tepla-Barrandian unit, Bohemian Massif2011 | Faculty of Science
- Plane-confined magnetic lineations in mingled mafic and felsic magmas, the Sazava pluton, Bohemian Massif2010 | Faculty of Science
- Multiple magmatic fabrics in plutons: an overlooked tool for exploring interactions between magmatic processes and regional deformation?2008 | Faculty of Science
- Multiple magmatic fabrics in the Sázava pluton (Bohemian Massif, Czech Republic): a result of superposition of wrench-dominated regional transpression on final emplacement2005 | 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
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