Classes
- 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 Course in GeodynamicsMG440T30 | 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
- 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
- The juxtaposition of eclogite and mid-crustal rocks in the Orlica-Snieznik Dome, Bohemian Massif2012 | Faculty of Science
- 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
- Microstructural and metamorphic evolution of a high-pressure granitic orthogneiss during continental subduction (Orlica-Snieznik dome, Bohemian Massif)2012 | 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
- Model of syn-convergent extrusion of orogenic lower crust in the core of the Variscan belt: implications for exhumation of high-pressure rocks in large hot orogens2011 | Faculty of Science
- Evolution of microstructure and melt topology in partially molten granitic mylonite: Implications for rheology of felsic middle crust2008 | Faculty of Science
- 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
Loading network view...