0145643 - GLU-S 20033014 RIV CZ eng J - Článek v odborném periodiku
Kučera, J. - Charvátová, K. - Hladil, Jindřich - Slobodník, M.
Hydrothermal mineralization in the Moravian Karst near Býčí skála Cave: post-Variscan deformation history?
Geolines. Roč. 16, Hrubá skála Chateau 2003, Proceedings of the 8th Meeting of the Czech Tectonic Studies Group / 1st Meeting of the Central European Tectonics Group, Hrubá skála Chateau Czech Republic. (2003), s. 66-67. ISSN 1210-9606.
[Meeting of the Czech Tectonic Studies Group /8./, Meeting of the Central European Tectonics Group, Hrubá skála Chateau /1./. Hrubá Skála, 24.04.2003-27.04.2003]
Grant CEP: GA AV ČR IAA3013209
Výzkumný záměr: CEZ:AV0Z3013912
Klíčová slova: carbonate veinlets * brittle deformation * Tertiary
Kód oboru RIV: DB - Geologie a mineralogie
Web výsledku:
http://geolines.gli.cas.cz/fileadmin/volumes/volume16/G16-066.pdf

The carbonate and quartz-carbonate veinlets in the Amphipora limestones (Devonian, Givetian) of the central Moravian Karst developed with a succession, where the younger generations have increased Mg-Fe-Mn abundances. The latest veins even contain sparse galena and barite. The hydrothermal veinlets developed during close pre-Badenian ages as a response to the brittle deformation of the Carpathian foreland. The magnetic and gamma-ray effects of these veinlets are slight, mostly in average of the host-rock values.
Trvalý link: http://hdl.handle.net/11104/0043209