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    Crystallographic preferred orientations of quartz and feldspar in post- and synkinematic emplaced granites
    The evolution of perpendicular linear fabrics in synkinematically emplaced tourmaline granite (central Moravia - Bohemian Massif)
    Magmatic history and geophysical signature of a post-collisional intrusive center emplaced near a crustal-scale shear zone: the Plechý granite pluton (Moldanubian batholith, Bohemian Massif)
    Magmatic history and geophysical signature of a post-collisional intrusive center emplaced nearby a crustal-scale shear zone: the Plechý granite pluton (Moldanubian batholith, Bohemian Massif)
    Magnetic fabric in granitoid plutons emplaced during Variscan orogeny and timing of their intrusions: Eastern Variscan front
    Multiple magmatic fabrics in episodically emplaced granites intranstensional setting: tectonic model based on AMS study and numerical modeling
    Neoproterozoic igneous complex emplaced along major tectonic boundary in the Kaoko Belt (NW Namibia) - ion probe and LA-ICPMS dating of magmatic and metamorphic zircons
    Neoproterozoic igneous complex emplaced along major tectonic boundary in the Kaoko Belt (NW Namibia): ion probe and LA-ICP-MS dating of magmatic and metamorphic zircons
    Neoproterozoic igneous complex emplaced along major tectonic boundary in the Kaoko Belt (NW Namibia): ion probe and LA-ICP-MS dating of magmatic and metamorphic zircons
    Neoproterozoic igneous complex emplaced along major tectonic boundary in the Kaoko Belt (NW Namibia): ion probe and LA-ICP-MS dating of magmatic and metamorphic zircons
    Reply to the comments on Magmatic history and geophysical signature of a post-collisional intrusive center emplaced near a crustal-scale shear zone: the Plechy´ granite pluton (Moldanubian batholith, Bohemian Massif)
    Tectonic evolution of a continental magmatic arc from transpression in the upper crust to exhumation of mid-crustal orogenic root recorded by episodically emplaced plutons: the Central Bohemian Plutonic Complex (Bohemian Massif)
    Tectonic evolution of a continental magmatic arc from transpression in the upper crust to exhumation of mid-crustal orogenic root recorded by episodically emplaced plutons: the Central Bohemian Plutonic Complex (Bohemian Massif)