Classes
- Field Course in GeodynamicsMG440T30 | Faculty of Science
- MOVE projectMG440C112 | Faculty of Science
- Structural GeologyMG440P17 | Faculty of Science
- Advanced Structural GeologyMG440P46 | Faculty of Science
- Magnetic Anisotropy and PaleomagnetismMG440P55 | Faculty of Science
- Numerical Modelling of Heat Transfer in GeologyMG440P73 | Faculty of Science
- Field Exercises in Structural GeologyMG440T68 | Faculty of Science
Publications
- Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: A numerical model2014 | Faculty of Science, Faculty of Mathematics and Physics
- Late Paleozoic-Mesozoic tectonic evolution of the Trans-Altai and South Gobi Zones in southern Mongolia based on structural and geochronological data2014 | Faculty of Science, Central Library of Charles University
- Kinematically unrelated C-S fabrics: an example of extensional shear band cleavage from the Veporic Unit (Western Carpathians)2013 | Faculty of Science
- A numerical model of exhumation of the orogenic lower crust in the Bohemian Massif during the Variscan orogeny2012 | Faculty of Science, Faculty of Mathematics and Physics
- Crustal influx, indentation, ductile thinning and gravity redistribution in a continental wedge: Building a Moldanubian mantled gneiss dome with underthrust Saxothuringian material (European Variscan belt)2012 | Faculty of Science
- Inverse ductile thinning via lower crustal flow and fold-induced doming in the West Carpathian Eo-Alpine collisional wedge2012 | Faculty of Science
- A geophysical model of the Variscan orogenic root (Bohemian Massif):Implications for modern collisional orogens2011 | Faculty of Science, Faculty of Mathematics and Physics
- Heat sources and trigger mechanisms of exhumation of HP granulites inVariscan orogenic root2011 | Faculty of Science, Faculty of Mathematics and Physics
- Prograde and retrograde metamorphic fabrics - a key for understanding burial and exhumation in orogens (Bohemian Massif)2011 | Faculty of Science
- Origin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny2011 | Faculty of Science
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