- Heat sources and trigger mechanisms of exhumation of HP granulites inVariscan orogenic root2011 | Faculty of Science, Faculty of Mathematics and Physics
- A geophysical model of the Variscan orogenic root (Bohemian Massif):Implications for modern collisional orogens2011 | Faculty of Science, Faculty of Mathematics and Physics
- The northern margin of the core of the Bohemian Massif (Processes at boundary of the orogenic root)1999 | Faculty of Mathematics and Physics, First Faculty of Medicine
- Magma emplacement during exhumation of lower- to mid-crustal orogenic root: the Jihlava syenitoid pluton, Moldanubian Unit, Bohemian Massif2006 | Faculty of Science
- The northern margin of the core of the Bohemian Massif (Processes at boundary of the orogenic root)1999 | Faculty of Science
- Fabric evolution in granulites and migmatites of the Variscan orogenic root (Bohemian Massif, Vosges) +1Publication without faculty affiliation
- Chronological constraints on the Palaeozoic geodynamic evolution of the Variscan orogenic root system: Moldanubian Zone of the Bohemian Massif2003 | Faculty of Science
- Chronological constraints on the Palaeozoic geodynamic evolution of the Variscan orogenic root system: Moldanubian Zone of the Bohemian Massif2003 | Faculty of Mathematics and Physics, First Faculty of Medicine
- Structures related to the exhumation of HP rocks within the orogenic root domain: examples of the SE moldanubian zone and the eastern Snieznik dome2001 | Faculty of Science
- 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
- 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
- Contrasting Early Carboniferous field geotherms - evidence for accretion of a thickened orogenic root and subducted Saxothuringian crust (Central European Variscides)2005 | Faculty of Science
- Thermally softened continental extensional zones (arcs and rifts) as precursors to thickened orogenic zones2001 | Faculty of Science
- Re-evaluation of polyphase kinematic and 40Ar/39Ar cooling history of Moldanubian hot nappe at the eastern margin of the Bohemian Massif2017 | Faculty of Science
- An Andean type Palaeozoic convergence in the Bohemian Massif2009 | Faculty of Science
- Tectonic evolution of a continental magmatic arc from transpression in the upper crust to exhumation of mid-crustal orogenic root recorded by episodically emplaced plutons: the Central Bohemian Plutonic Complex (Bohemian Massif)2005 | Faculty of Science
- Structural position of high-pressure felsic to intermediate granulites from NE Moldanubian domain (Bohemian Massif)2010 | 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
- From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif)2008 | Faculty of Science, Central Library of Charles University
- 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
- Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: A numerical model2014 | Faculty of Science, Faculty of Mathematics and Physics
- Importance of crustal relamination in origin of the orogenic mantle peridotite–high-pressure granulite association: example from the Náměšť Granulite Massif (Bohemian Massif, Czech Republic)2015 | Central Library of Charles University
- 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
- High-Ti muscovite as a prograde relict in high pressure granulites with metamorphic Devonian zircon ages (Běstvina granulite body, Bohemian Massif): Consequences for the relamination model of subducted crust2014 | 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
- Finite pattern of Barrovian metamorphic zones: interplay between thermal reequilibration and post-peak deformation during continental collision-insights from the Svratka dome (Bohemian Massif)2020 | Faculty of Science
- Decoupling of Mg from Sr-Nd isotopic compositions in Variscan subduction-related plutonic rocks from the Bohemian Massif: implications for mantle enrichment processes and genesis of orogenic ultrapotassic magmatic rocks2022 | Faculty of Science, Central Library of Charles University
- Ultrapotassic magmatism in the heyday of the Variscan Orogeny: the story of the Trebic Pluton, the largest durbachitic body in the Bohemian Massif2020 | Faculty of Science, Central Library of Charles University