Podrobnosti záznamu

Předmětová skupina
    analýza petrotektonická
    The acid metavolcanic rocks of the Orlica-Śnieżnik Dome (Sudetes): their origin and tectono-metamorphic evolution
    Amfibolické kvarcity s L-stavbou ze zóny Červenohorského sedla (Hrubý Jeseník) (14-24, Bělá pod Pradědem)
    Analogue and numerical modelling of shape fabrics: consequences for strain and flow determination in magmas
    Cadomian versus Variscan fabrics in the Desná dome basement rocks, East Sudetes
    Calcite Mylonites of SW Brunovistulicum
    Conjugate shear zones in the Southern Bohemian Massif (Austria): implications for Variscan and Alpine tectonothermal activity
    Constriction due to subduction: evidence for slab pull in the Mariánské Lázně complex (central European Variscides)
    Contrasting P-T conditions during conjugate shear zone development in the Southern Bohemian Massif, Austria
    Contrasting textural record of two distinct metamorphic events of similar P-T conditions and different durations
    Deformation of inhomogenous calcite aggregates: an example from Variscan limestones of Moravia
    Deformation phases in the southern Bavarian Forest: constraints from sheared granitoids
    Destruction of orthogneiss layered structure through partial melting and melt infiltration in high temperature shear zone: quantitative textural study of anatectic process
    The development of mid-crustal extensional shear zone during Cretaceous convergence of the Vepor Unit in the West Carpathians
    Development of the Gföhl Migmatites through Partial Melting and Textural Annealing of High-Grade Orthogneiss via Process of Disintegration of Solid State Texture
    From extension to compression: Late Miocene stress inversion in the Alpine-Carpathian-Pannonian transition area
    Generacje mikrostruktur w łupkach ilasto-piaszczystych formacji andelskohorskiej (Sudety Wschodnie, Polska)
    Infiltration of silicate melts in to [p.e. into] the continental crust: microstructural, thermodynamic and geochemical approach
    Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root: example of the Blanský les granulite, Bohemian Massif, Czech Republic
    Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root: example of the Blanský les granulite, Bohemian Massif, Czech Republic
    Konjugierte Scherzonen in der südlichen Böhmischen Masse: variszische und alpidische kinematische Entwicklungen, Projekt S4713
    Late-orogenic extension in the Bohemian Massif: Petrostructural evidence in the Hlinsko region
    Late Variscan stress-field rotation initiating escape tectonics in the south-western Bohemian Massif: a far field response to late-orogenic extension
    Late Variscan strike-slip tectonics between the Teplá-Barrandien and Moldanubian terranes (Czech Bohemian Massif): petrostructural evidence
    Metamorphic and microstructural evolution of orthogneisses and granulites of the Eger complex (NW Bohemian Massif) - record of progressive granulitization of the lower crust?
    Microfabric of fresh and weathered marbles: Implications and consequences for the reconstruction of the Marborpalais Potsdam
    Microstructural record of an orogen-parallel extension in the Vepor Unit, West Carpathians
    On the genesis of two meridionally trending lineations in rocks of the Orlica-Śnieżnik Dome: evidence from marbles of the Stronie formation
    Origin and orientation of microporosity in eclogites of different microstructure
    Origin of felsic migmatites by ductile shearing and melt infiltration
    Origin of migmatites by deformation-enhanced melt infiltration of orthogneiss: a new model based on quantitative microstructural analysis
    Perpendicular linear fabrics in granite: markers of combined simple shear and pure shear flows : qranite: From Segregation of Melt to Emplacement Fabrics
    Petrostrukturní vztahy metamorfovaných a magmatických hornin v oblasti Nové Pece a Trojmezí (Moldanubikum, Šumava)
    Quantitative Textural and Microstructural Study of Orthogneiss Deformed during Continental Underthrusting
    Quantitative textural and microstructural study of orthogneiss deformed during continental underthrusting: result of contrasting mineral rheologies and solid state annealing
    Quartz c-axis fabrics in constrictionally strained orthogneisses: implications for the evolution of the Orlica-Śnieżnik Dome, the Sudetes, Poland
    Quartz-texture evolution within an orthogneiss structure (Reitzenhain structure, Erzgebirge, SE-Germany), determined by neutron-difraction- The case of fabric isotropization under granitization
    Rheology of granitoids deformed at Barrovian metamorphic field gradient in different crustal levels
    Rocks deformed in the constrictional regime: L>S to L tectonites in the Orlica-Śnieżnik Dome, the Sudetes, Poland
    Strain fabric of the upper mantle rocks and their emplacement into high-pressure granulite in the Kutná hora crystalline complex, Bohemian massif
    Structure elements of Rocks and energy-frequency distribution of seismic phenomena
    Strukturní vývoj metagranitů ze svrateckého krystalinika
    Syntectonic Lower Ordovician migmatite and post-tectonic Upper Viséan syenite in the western limb of the Orlica-Śnieżnik Dome, West Sudetes: U-Pb SHRIMP data from zircons
    Tectonic and Stratigraphic Study of Limestones at the Western Border of the Brno Massif
    Tectonometamorphic evolution of the Svratka Crystalline Complex (NE Bohemian Massif) : evidence for wrench-dominated tranpression [transpression] along the NE margin of the Variscan orogenic root
    Two types of "augen gneisses" in the Śnieżnik Metamorphic Unit, West Sudetes, Poland
    A Variscan continental collision of the West Sudetes and the Brunovistulian terrane: a contribution from structural and metamorphic record of the Stronie Formation, the Orlica-Śnieżnik Dome, SW Poland
    Vznik a vývoj metagranitů svrateckého krystalinika : 14-33 Polička, 24-11 Nové Město na Moravě
    Zawidów granodiorite from the Lusatian massif in SW Poland
    Zur tektonometamorphen Entwicklung der Zentralböhmischen Scherzone zwischen Svatá Kateřina und Rittsteig unter besonderer Berücksichtigung der Forschungsbohrung Rittsteig (Böhmische Masse)