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
- Elastic anisotropy and pore space geometry of schlieren granite: direct 3-D measurements at high confining pressure combined with microfabric analysis2013 | Faculty of Science
- Kinematically unrelated C-S fabrics: an example of extensional shear band cleavage from the Veporic Unit (Western Carpathians)2013 | Faculty of Science
- 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
- Microstructural and metamorphic evolution of a high-pressure granitic orthogneiss during continental subduction (Orlica-Snieznik dome, Bohemian Massif)2012 | 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
- Origin of migmatites by deformation-enhanced melt infiltration of orthogneiss: a new model based on quantitative microstructural analysis2008 | Faculty of Science, Central Library of Charles University
- 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
- Microstructural-deformation record of an orogen-parallel extension in the Vepor Unit, West Carpathians2007 | 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
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