Based on combined microthermometric/isotopic study Variscan hydrothermal veins of the Prague Synform crystallised in a geochemically closed system from relatively low-salinity fluids connected with host-rocks during conditions of the oil window.
Based on combined microthermometric/isotopic study Variscan hydrothermal veins of the Prague Synform crystallised in a geochemically closed system from relatively low-salinity fluids connected with host-rocks during conditions of the oil window. (en)
CzechTec07 - 5th Meeting of the Central European Tectonic Studies Group and 12th Meeting of the Czech tectonic Studies Group, April 11-14, 2007, Teplá, Czech Republic