Classes
- Structural GeologyMG440P17 | Faculty of Science
- MOVE projectMG440C112 | 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 Course in GeodynamicsMG440T30 | Faculty of Science
- Field Exercises in Structural GeologyMG440T68 | Faculty of Science
Publications
- 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
- Extreme ductile deformation of fine-grained salt by coupled solution-precipitation creep and microcracking: Microstructural evidence from perennial Zechstein sequence (Neuhof salt mine, Germany)2012 | Faculty of Science, Central Library of Charles University
- Inverse ductile thinning via lower crustal flow and fold-induced doming in the West Carpathian Eo-Alpine collisional wedge2012 | Faculty of Science
- Heat sources and trigger mechanisms of exhumation of HP granulites inVariscan orogenic root2011 | Faculty of Science, Faculty of Mathematics and Physics
- 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
- Vertical extrusion and horizontal channel flow of orogenic lower crust: key exhumation mechanisms in large hot orogens?2008 | Faculty of Science, Central Library of Charles University
- Extreme ductility of feldspar aggregates - Melt enhanced grain boundary sliding and creep failure: Rheological implications for felsic lower crust2007 | Faculty of Science, Central Library of Charles University
- Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root: example of the Blansky les granulite, Bohemian Massif, Czech Republic2006 | Faculty of Science
- The quantitative link between fold geometry, mineral fabric and mechanical anisotropy: as exemplified by the deformation of amphibolites across a regional metamorphic gradient2005 | Faculty of Science, Central Library of Charles University
- Contrasting microstructure and deformation mechanisms in metagabbro mylonites contemporaneously deformed under different temperatures (c. 650°C and c. 750°C)2005 | Faculty of Science
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