Podrobnosti záznamu

Jméno
   Lexa, O.
Autor článku
   An Andean type Palaeozoic convergence in the Bohemian Massif
   Contrasting microstructures and deformation mechanisms in metagabbro mylonites contemporaneously deformed under different temperatures (c. 650 °C and c. 750 °C)
   Elastic anisotropy and pore space geometry of schlieren granite: direct 3-D measurements at high confining pressure combined with microfabric analysis
   Emplacement dynamics of phonolite magma into maar-diatreme structures - Correlation of field, thermal modeling and AMS analogue modeling data
   Evolution of microstructure and melt topology in partially molten granitic mylonite: implications for rheology of felsic middle crust
   Extreme ductility of feldspar aggregates - Melt-enhanced grain boundary sliding and creep failure: Rheological implications for felsic lower crust
   Geology of Trans-Altai Gobi, SW Mongolia
   The mechanism of flow and fabric development in mechanically anisotropic trachyte lava
   The mechanism of flow and fabric development in mechanically anisotropic trachyte lava
   Metamorphic record of high temperature interaction between mantle rocks and felsic granulites
   Noncoaxial K-feldspar and AMS subfabrics in the Land's End granite, Cornwall: Evidence of magmatic fabric decoupling during late deformation and matrix crystallization
   Origin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny
   Origin of migmatites by deformation-enhanced melt infiltration of orthogneiss: a new model based on quantitative microstructural analysis
   Origin of migmatites by deformation-enhanced melt infiltration of orthogneiss: a new model based on quantitative microstructural analysis