- Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: A numerical model2014 | Faculty of Science, Faculty of Mathematics and Physics
- Carboniferous exhumation of thickened lower crust through wedge tectonics and subsequent lateral spreading in the middle crust: Moldanubian zone of the Bohemian Massif2003 | Faculty of Science
- Geophysical and geochemical nature of relaminated arc-derived lower crust underneath oceanic domain in southern Mongolia2015 | 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
- 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
- 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
- Petrology and geochemistry of lower crust in Bohemian Massif: two contrasting lithospheres1996 | Faculty of Mathematics and Physics, First Faculty of Medicine
- Thermal evolution of the orogenic lower crust during exhumation within a thickened Moldanubian orogenic root of the Variscan belt of Central Europe2006 | Faculty of Science
- Carboniferous exhumation of thickened lower crust through wedge tectonics and subsequent lateral spreading in the middle crust: Moldanubian zone of the Bohemian Massif2003 | Faculty of Mathematics and Physics, First Faculty of Medicine
- Granulites and granulites 2009 - Granulites, partial melting and rheology of orogenic lower crust2009 | Faculty of Science
- Strain coupling between upper mantle and lower crust: natural example from the Běstvina granulite body, Bohemian Massif2009 | Faculty of Science
- Computational study of deformation mechanisms and grain size evolution in granulites - Implications for the rheology of the lower crust2017 | Faculty of Science
- Exhumation of the Blanský Les Granulite Massif as a Result of Oblique Thrusting and Crustal-Scale Buckling2003 | Faculty of Science
- A Mechanism for Syn-Convergent Exhumation of HP Granulites in the Bohemian Massif, Czech Republic: Geochronological, Structural and Petrological Constraints2003 | Faculty of Science
- Structural position of high-pressure felsic to intermediate granulites from NE Moldanubian domain (Bohemian Massif)2010 | Faculty of Science
- Juxtaposition of Barrovian and migmatite domains in the Chinese Altai: a result of crustal thickening followed by doming of partially molten lower crust2015 | Faculty of Science
- Structure and Episodic Tectonic Evolution of the Lower Crustal Accretionary Wedge in Moldanubian Zone, Austria2003 | 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
- High-temperature fracturing and subsequent grain-size-sensitive creep in lower crustal gabbros: Evidence for coseismic loading followed by creep during decaying stress in the lower crust?2015 | 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
- Magmatic fabrics and emplacement of the cone-sheet-bearing Knížecí Stolec durbachitic pluton (Moldanubian Unit, Bohemian Massif): implications for mid-crustal reworking of granulitic lower crust in the Central European Variscides2008 | Faculty of Science
- Fingerprinting sources of orogenic plutonic rocks from Variscan belt with lithium isotopes and possible link to subduction-related origin of some A-type granites2010 | Faculty of Science
- Clinopyroxene from an alkali pyroxenite xenolith, Loucna-Oberwiesenthal Volcanic Centre, Bohemian Massif: crystal chemistry and structure2006 | Faculty of Science
- Magmatic Tempos in Large Hot Orogens in Comparison with Continental Margin Arcs2020 | Faculty of Science
- Trans-lithospheric diapirism explains the presence of ultra-high pressure rocks in the European Variscides2021 | Faculty of Science
- European Variscan orogenic evolution as an analogue of Tibetan-Himalayan orogen: Insights from petrology and numerical modeling2016 | Faculty of Science, Faculty of Mathematics and Physics
- Exhumation of the Blanský Les Granulite Massif as a Result of Oblique Thrusting and Crustal-Scale Buckling2003 | Faculty of Mathematics and Physics, First Faculty of Medicine
- A Mechanism for Syn-Convergent Exhumation of HP Granulites in the Bohemian Massif, Czech Republic: Geochronological, Structural and Petrological Constraints2003 | Faculty of Mathematics and Physics, First Faculty of Medicine
- Structure and Episodic Tectonic Evolution of the Lower Crustal Accretionary Wedge in Moldanubian Zone, Austria2003 | Faculty of Mathematics and Physics, First Faculty of Medicine
- Inverse ductile thinning via lower crustal flow and fold-induced doming in the West Carpathian Eo-Alpine collisional wedge2012 | Faculty of Science