Podrobnosti záznamu

   Schulmann, K.
Autor článku
   AMS record of brittle dilation, viscous-stretching and gravity-driven magma ascent in area of magma-rich crustal extension (Vosges Mts., NE France)
   An Andean type Palaeozoic convergence in the Bohemian Massif
   Anisotropy of magnetic susceptibility of the multiphase intrusion if the Nasavrky plutonic complex: structural implication
   Contrasting microstructures and deformation mechanisms in metagabbro mylonites contemporaneously deformed under different temperatures (c. 650 °C and c. 750 °C)
   Crustal influx, indentation, ductile thinning and gravity redistribution in a continental wedge: Building a Moldanubian mantled gneiss dome with underthrust Saxothuringian material (European Variscan belt)
   Ductile deformation and rheology of sub-continental mantle in a hot collisional orogeny: Example from the Bohemian Massif
   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
   Internal fabric development in complex lava domes
   The juxtaposition of eclogite and mid-crustal rocks in the Orlica-Snieznik Dome, Bohemian Massif
   The mechanism of flow and fabric development in mechanically anisotropic trachyte lava
   Microstructural and metamorphic evolution of a high-pressure granitic orthogneiss during continental subduction (Orlica-Snieznik dome, Bohemian Massif)
   Microstructure mechanism map of dynamically recrystallized marble
   Model of successive granite sheet emplacement in transtensional setting: Integrated microstructural and anisotropy of magnetic susceptibility study
   Non-scaled analogue modelling of AMS development during viscous flow: a simulation on diapir-like structures
   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
   What does AMS tell us about emplacement of granites: Comparative K-feldspar and AMS fabric study