Podrobnosti záznamu

Předmětová kategorie
    stress field
Článek
    Apatite fission track implications for timing of hydrothermal fluid flow in Tertiary volcanics of the Bohemian Massif
    Evidence for non-coaxiality of ferrimagnetic and paramagnetic fabrics, developed during magma flow and cooling in a thick mafic dyke
    S-wave splitting from records of local micro-earthquakes in West Bohemia/Vogtland: an indicator of complex crustal anisotropy
    Time succession of Cenozoic stress fields in the northern part of the Bohemian Massif