CLR person interests, research and publications
Researcher

About me
Primarily, my main job consists in studying petrology, geochemistry and petrogenesis of igneous and metamorphic rocks. They come mostly from Bohemian Massif, but we have had also projects in Sierra Nevada, Nicaragua, Namibia or Antarctic Peninsula. Apart from that, we are busy developing free tools for interpretation and graphical presentation of geochemical data. My pet are granitoids (and Hercynian granitoids of the Central Bohemian Pluton in particular). Since 2002 I have been involved in a project dealing with petrogenesis of South Bohemian granulites. Arguably the most important project I have been involved in is the open-access journal of the Czech Geological Society, since 2007 published under the name Journal of Geosciences.
Research interests
- Petrology, geochemistry and petrogenesis of granitoid rocks geochemistry and genesis of Variscan granulites
- Rb–Sr and Sm–Nd geochronology (magmatic as well as metamorphic rocks)
- Sr and Nd isotopes in petrogenetic studies
- Strontium chemostratigraphy
- Numerical modelling in igneous geochemistry, computing in geosciences
Research projects
Melting of the crust leads to granitic magmas that vary widely in composition and in ability to generate metal deposits or cause explosive volcanism. A number of superposing, competing processes control this variability. Much has been learnt from investigating processes late in the magma history, but not much is known about magma generation at depth and what happens to it during transport to the upper crust. Indirect knowledge or inferences based on little data, leads to speculation and controversies.
Selected segments of Euroasian orogenic system are used to constrain relative contribution of contrasting processes of continental construction in collisional and accretionary orogenic systems. Principal objectives of the proposal are: (i) identification of the individual terranes, kinematic analysis of their movements and characterization of deformation style connected with their amalgamation; (ii) estimation of net crustal growth vs. recycling of preexistent crustal material.
On the modern Earth, continental crust is created mainly at subduction zones. Here, release of aqueous fluid from dehydrating oceanic crust causes melting in the mantle wedge and generates the calc-alkaline magmas that evolve into granitoid continental crust. This project aims to understand crustal growth and possible crustal construction mechanisms, using the Mongolian and Chinese tract of the Central Asian Orogenic Belt (CAOB) as an example. The main questions raised here are: What were the cause, rate and timing of continental growth in the CAOB?