Classes
- 3D modeling in geologyMG420P12 | Faculty of Science
- GIS and remote sensing in geologyMG421P41 | Faculty of Science
- Computer processing of geoscience dataMG421C02 | Faculty of Science
- Sedimentary PetrologyMG421P13 | Faculty of Science
- Principles of petrology of sedimentary rocksMG421P39 | Faculty of Science
- Excursion of sedimentary geologyMG421T15 | Faculty of Science
Publications
- Neogene-Quaternary response of the Novohradske hory Mts. (Czech Republic) fluvial systems to tectonics - Analyses of morphotectonics, stream-length index and structural geology2023 | Faculty of Science
- Evaluation of Climatic and Tectonic Imprints In Fluvial Successions of An Early Permian Depositional System (Asselian Vrchlabí Formation, Krkonoše Piedmont Basin, Czech Republic)2022 | Faculty of Science
- Main Ethiopian Rift landslides formed in contrasting geological settings and climatic conditions2021 | Faculty of Science, Central Library of Charles University
- Geochemical history of a Lower Miocene lake, the Cypris Formation, Sokolov Basin, Czech Republic2017 | Faculty of Science, Central Library of Charles University
- Significant hiatuses in the terrestrial Late Variscan Central and Western Bohemian basins (Late Pennsylvanian-Early Cisuralian) and their possible tectonic and climatic links2017 | Faculty of Science
- A review of the Middle-Late Pennsylvanian west European regional substages and floral biozones, and their correlation to the Global Time Scale based on new U-Pb ages2016 | Faculty of Science
- The Main Ostrava Whetstone: composition, sedimentary processes, palaeogeography and geochronology of a major Mississippian volcaniclastic unit of the Upper Silesian Basin (Poland and Czech Republic)2013 | Faculty of Science
- Castle Conglomerate Unit of the Upper Silesian Basin (Czech Republic and Poland): a record of the onset of Late Mississippian C2 glaciation?2013 | Faculty of Science
- Lacustrine carbonates of Ploužnice Level, Stephanian C, Krkonoše Piedmont Basin2013 | Faculty of Science
- Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia2012 | Faculty of Science
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