- Mantle-derived, UHP garnet pyroxenite and eclogite in the Moldanubian Gfohl nappe, Bohemian Massif : A geochemical review, new P-T determinations and tectonic interpretation2006 | Faculty of Science
- Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt-rock reactions2009 | Faculty of Science
- Re-Os and Lu-Hf isotopic constraints on the formation and age of mantle pyroxenites from the Bohemian Massif2016 | Faculty of Science, Central Library of Charles University
- Petrology and geochemical characteristics of phlogopite pyroxenite related to durbachites, Moldanubian Zone, Bohemian Massif2015 | Faculty of Science
- Garnet pyroxenite in the Biskupice peridotite, Bohemian Massif: anatomy of a Variscan high-pressure cumulate2013 | Faculty of Science
- Eclogite, Garnet Peridotite, Garnet Pyroxenite and HP Granulite2011 | Faculty of Science
- Petrological, Geochemical and Sr-Nd-O Isotopic Constraints on the Origin of Garnet and Spinel Pyroxenites from the Moldanubian Zone of the Bohemian Massif2016 | Faculty of Science, Central Library of Charles University
- High-pressure crystallization vs. recrystallization origin of garnet pyroxenite-eclogite within subduction related lithologies2018 | Faculty of Science
- Clinopyroxene from an alkali pyroxenite xenolith, Loucna-Oberwiesenthal Volcanic Centre, Bohemian Massif: crystal chemistry and structure2006 | Faculty of Science
- Highly siderophile element geochemistry of peridotites and pyroxenites from Horni Bory, Bohemian Massif: Implications for HSE behaviour in subduction-related upper mantle2013 | Faculty of Science
- Garnet pyroxenite and eclogite in the Bohemian Massif : geochemical evidence for Variscan recycling of subducted lithosphere1995 | First Faculty of Medicine, Faculty of Mathematics and Physics
- Subduction of lithospheric upper mantle recorded by solid phase inclusions and compositional zoning in garnet: Example from the Bohemian Massif2013 | Faculty of Science
- Magnetic fabrics in garnet peridotites-pyroxenites and host felsic granulites in the South Bohemian Granulites (Czech Republic): Implications for distinguishing between primary and metamorphism induced fabrics2013 | Faculty of Science
- Compositional trends in Ba-,Ti-, and Cl-rich micas from metasomatized mantle rocks of Gföhl Unit, Bohemian Massif, Austria2023 | Faculty of Science
- South Bohemian HP Granulites with Lenses of HP/UHP Mafic and Ultramafic Rocks2011 | Faculty of Science, Central Library of Charles University
- Garnet exsolution in pyroxene from clinopyroxenites in the Moldanubian zone: constraining the early pre-convergence history of ultramafic rocks in the Variscan orogen2009 | Faculty of Science
- Eclogite and Garnet Clinopyroxenite from Monotonous Unit2011 | Faculty of Science
- Depletion, cryptic metasomatism, and modal metasomatism (refertilization) of Variscan lithospheric mantle: Evidence from major elements, trace elements, and Sr-Nd-Os isotopes in a Saxothuringian garnet peridotite2015 | Faculty of Science
- An internally consistent pressure calibration of geobarometers applicable to the Earth's upper mantle using in situ XRD2018 | Faculty of Science
- Highly siderophile element geochemistry and Re-Os isotopic systematics of carbonatites: Insights from Tamil Nadu, India2019 | Faculty of Science, Central Library of Charles University
- On the Chemical Composition and Possible Origin of Na-Cr-Rich Clinopyroxene in Silicocarbonatites from Samalpatti, Tamil Nadu, South India2018 | 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
- Petrogenesis and Lu-Hf Dating of (Ultra)Mafic Rocks from the Kutna Hora Crystalline Complex: Implications for the Devonian Evolution of the Bohemian Massif2020 | Faculty of Science
- High-temperature overprint in (U)HPM rocks exhumed from subduction zones; A product of isothermal decompression or a consequence of slab break-off (slab rollback)?2020 | Faculty of Science