Podrobnosti záznamu

Klíčové slovo
    E-W
Článek
    Perpendicular fabrics in the Orlické hory orthogneisses (western part of the Orlice-Sněžník Dome, Bohemian Massif) due to high temperature E-W deformational event and late lower temperature N-S overprint
    Variscan tectonics of allochthonous units of the Erzgebirge and the Vogtland (Saxo-Thuringian Zone): An E-W profile from the gneiss dome of Reitzenhain to the Berga antiform