National Repository of Grey Literature 3 records found  Search took 0.01 seconds. 
From microstructures to large-scale crustal deformations in collisional orogen: multidisciplinary approach
Franěk, Jan ; Schulmann, Karel (advisor) ; Faryad, Shah Wali (referee) ; Stünitz, Holger (referee) ; Whitechurch, Hubert (referee)
The thesis aims to compile response of deep-seated rocks to continental collision in the root zone of Variscan orogen exposed in Bohemian Massif. It treats the orogenic processes from the scale of microscopic grains constituting rocks through scale of individual outcrops to an overall view of ~4000 km2 large domain of the high-grade rocks. The thesis is divided into three chapters. The first represents an article summarizing study of structurally most complex area - Blanský les granulite massif - published in the Mineralogy and Petrology journal (2006). The second chapter unravels regional evolution of the south Bohemian Moldanubian domain and correlates the presented results with suitable studies from other orogenic regions or with numerical models of continental collisions. The related article will be submitted to Tectonics journal in June 2007. The last section focuses on the mechanisms of deformation in the felsic granulites and extrapolates the results to rheology of the Variscan lower crust and behavior of common felsic rocks under HT HP conditions. The corresponding paper will be submitted to Journal of Metamorphic Geology in the autumn 2007. The Bohemian massif represents the easternmost exposure of Variscan orogen in Europe. During the 380-300 Ma complex subduction - collision a ~300km...
From microstructures to large-scale crustal deformations in collisional orogen: multidisciplinary approach
Franěk, Jan ; Schulmann, Karel (advisor) ; Faryad, Shah Wali (referee) ; Stünitz, Holger (referee) ; Whitechurch, Hubert (referee)
The thesis aims to compile response of deep-seated rocks to continental collision in the root zone of Variscan orogen exposed in Bohemian Massif. It treats the orogenic processes from the scale of microscopic grains constituting rocks through scale of individual outcrops to an overall view of ~4000 km2 large domain of the high-grade rocks. The thesis is divided into three chapters. The first represents an article summarizing study of structurally most complex area - Blanský les granulite massif - published in the Mineralogy and Petrology journal (2006). The second chapter unravels regional evolution of the south Bohemian Moldanubian domain and correlates the presented results with suitable studies from other orogenic regions or with numerical models of continental collisions. The related article will be submitted to Tectonics journal in June 2007. The last section focuses on the mechanisms of deformation in the felsic granulites and extrapolates the results to rheology of the Variscan lower crust and behavior of common felsic rocks under HT HP conditions. The corresponding paper will be submitted to Journal of Metamorphic Geology in the autumn 2007. The Bohemian massif represents the easternmost exposure of Variscan orogen in Europe. During the 380-300 Ma complex subduction - collision a ~300km...
Tectonic evolution of the central part of the Teplá-Barrandian unit
Hajná, Jaroslava ; Žák, Jiří (advisor) ; Schulmann, Karel (referee) ; Nance, Damian (referee)
The principal goal of the thesis is to examine the tectonic evolution of the Teplá- Barrandian unit (TBU) of the central Bohemian Massif from Cadomian subduction and active margin processes, through Cambro-Ordovician extension to Variscan terrane collisions. The thesis is based on extensive field research, detailed structural mapping, and structural analysis, combined with other analytical methods such as the anisotropy of magnetic susceptibility (AMS) coupled with an analysis of magnetic mineralogy, analysis of deformational microstructures, and U, Th and Pb isotope analyses carried out by laser ablation - inductively coupled plasma-mass spectrometry (LA-ICP-MS). The most important conclusions of the thesis are as follows. (1) The Neoproterozoic (Cadomian) basement of the Teplá-Barrandian unit reveals a complex structure and mostly unclear stratigraphic relations of its components. It was proposed that this unit exposes perhaps the best preserved fragment of an accretionary wedge of the whole Avalonian-Cadomian belt, represented by the newly defined Blovice Complex. In the central part of the TBU, this complex consists of three lithotectonic belts differing in style and intensity of deformation, magnetic fabric, and degree of Cadomian regional metamorphism. In addition, the central...

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