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crust
Person
Class
Person
Publication
Programmes
Mgr. Martin Racek Ph.D.
Academic staff at Faculty of Science
2 classes
41 publications
Classes
class
Microanalysis of Geomaterials
MG440C79 |
Faculty of Science
class
Fundamentals of Electron Microscopy and Microanalysis
MG440P63 |
Faculty of Science
Publications
publication
Compositional trends in Ba-,Ti-, and Cl-rich micas from metasomatized mantle rocks of Gföhl Unit, Bohemian Massif, Austria
2023 |
Faculty of Science
publication
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
publication
Effects of diffusion of water and migration of melts in crustal rocks: An experimental study
2020 |
Faculty of Science
publication
Role of strain localization and melt flow on exhumation of deeply subducted continental crust
2018 |
Faculty of Science, Central Library of Charles University
publication
Juxtaposition of Barrovian and migmatite domains in the Chinese Altai: a result of crustal thickening followed by doming of partially molten lower crust
2015 |
Faculty of Science
publication
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 crust
2014 |
Faculty of Science
publication
Heat sources and trigger mechanisms of exhumation of HP granulites inVariscan orogenic root
2011 |
Faculty of Science, Faculty of Mathematics and Physics
publication
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
publication
Metamorphic record of burial and exhumation of orogenic lower and middle crust: a new tectonothermal model for the Drosendorf window (Bohemian Massif, Austria)
2006 |
Faculty of Science
publication
Carboniferous exhumation of thickened lower crust through wedge tectonics and subsequent lateral spreading in the middle crust: Moldanubian zone of the Bohemian Massif
2003 |
Faculty of Science
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