Podrobnosti záznamu

Jméno
   Hasalová, Pavlína
Autor článku
   Can the pervasive melt flow work in the crust? Microstructural, petrological and geochemical arguments from the Variscan Gföhl orthogneiss-migmatite complex, Bohemian Massif
   Clasts rotation and nature of strain localozation in thick ultramylonites: the el Pichao shear Zone, NW Argentina.
   Destruction of orthogneiss layered structure through partial melting and melt infiltration in high temperature shear zone: quantitative textural study of anatectic process
   Development of the Gföhl Migmatites through Partial Melting and Textural Annealing of High-Grade Orthogneiss
   Development of the Gföhl Migmatites through Partial Melting and Textural Annealing of High-Grade Orthogneiss
   Development of the Gföhl Migmatites through Partial Melting and Textural Annealing of High-Grade Orthogneiss via Process of Disintegration of Solid State Texture
   From orthogneiss to migmatite: geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif)
   From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif)
   Geochemical and geochronological arguments for heterogeneous nature and complex development of Variscan lower continental crust: Náměšť Granulite Massif (Bohemian Massif, Czech Republic)
   Geochemical and geochronological arguments for heterogeneous nature and complex development of Variscan lower continental crust: Náměšť Granulite Massif (Bohemian Massif, Czech Republic)
   Heterogeneity of the Variscan lower continental crust and upper mantle: whole-rock geochemistry and isotopic data from the Náměšť Granulite Massif (Bohemian Massif, Czech Republic)
   Infiltration of silicate melts in to [p.e. into] the continental crust: microstructural, thermodynamic and geochemical approach
   Influence of melt induced mechanical anisotropy on the magnetic fabrics and rheology of deforming migmatites, Central Vosges, France
   Interaction between deformation and magma extraction in migmatites: Examples from Kangaroo Island, South Australia
   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
   Origin of migmatites by deformation-enhanced melt infiltration of orthogneiss: a new model based on quantitative microstructural analysis
   Reactive porous flow and formation of infiltration migmatites: microstructural and petrological approach
   The role of melt infiltration in the formation of migmatitic orthogneiss
   Transformation of mylonitic metagranite to migmatite by open-system interactions during melt flow: an example from the Gföhl Unit (Bohemian Massif)
   Transformation of mylonitic metagranite to migmatite by open-system interactions during melt flow: an example from the Gföhl Unit (Bohemian Massif)
   Transforming mylonitic metagranite by open-system interactions during melt flow
   Transforming mylonitic metagranite by open-system interactions during melt flow
   Transforming mylonitic metagranite by open-system interactions during melt flow
   Transforming mylonitic metagranite to migmatite by open-system interactions during melt flow