Classes
- Microscopy of Minerals and Rocks for TeachersMG440C11 | Faculty of Science
- Microscopy of Rocks +1MG440C12 | Faculty of Science
- Fundamentals of PetrologyMG440P04 | Faculty of Science
- Petrology of Metamorphic Rocks +1MG440P10 | Faculty of Science
- Advanced Metamorphic PetrologyMG440P35 | Faculty of Science
- Materials Forming the Earth's CrustMG440P74 | Faculty of Science
Publications
- Magnetic fabrics in garnet peridotites-pyroxenites and host felsic granulites in the South Bohemian Granulites (Czech Republic): Implications for distinguishing between primary and metamorphism induced fabrics2013 | Faculty of Science
- Determination of field-independent and field-dependent components of anisotropy of susceptibility through standard AMS measurement in variable low fields II:2009 | Faculty of Science
- Primary magnetic fabric in an ultramafic body (Moldanubian Zone, European Variscides) survives exhumation-related granulite-amphibolite facies metamorphism2009 | Faculty of Science
- Constraining the P-T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)2022 | Faculty of Science
- Advantages and Limitations of Combined Diffusion-Phase Equilibrium Modelling for Pressure-Temperature-Time History of Metamorphic Rocks2022 | Faculty of Science
- Dissolution and Reprecipitation of Garnet during Eclogite-facies Metamorphism; Major and Trace Element Transfer during Atoll Garnet Formation2021 | Faculty of Science
- High-temperature overprint in (U)HPM rocks exhumed from subduction zones; A product of isothermal decompression or a consequence of slab break-off (slab rollback)?2020 | Faculty of Science
- Multi-stage metamorphism by progressive accretion of continental blocks, example from the Western Hindu Kush +12020 | Faculty of Science
- Pre-Alpine high-pressure metamorphism in the Gemer unit: mineral textures and their geodynamic implications for Variscan Orogeny in the Western Carpathians2020 | Faculty of Science
- Mineral textures of olivine minette and their significance for crystallization history of parental magma; an example from the Moldanubian Zone (the Bohemian Massif)2019 | Faculty of Science
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