Retrográdně-metamorfní a hydrotermální alterace hornin na uranovém ložisku Rožná

Warning

This publication doesn't include Faculty of Sports Studies. It includes Faculty of Science. Official publication website can be found on muni.cz.

Title in English	Retrograde-metamorphic and hydrothermal alterations at the Rožná uranium deposit
Authors	KŘÍBEK Bohdan ŽÁK Karel SULOVSKÝ Petr PUDILOVÁ Marta ZIMÁK Jiří
Year of publication	2002
Type	Article in Proceedings
Conference	Zprávy o geologických výzkumech v roce 2001
MU Faculty or unit	Faculty of Science
Citation
Field	Geology and mineralogy
Keywords	Alterations; Rožná uranium deposit; K/Ar dating; H and O isotopes; chlorite; geochemistry
Description	The Rožná uranium deposit is located in cataclastites that formed during Late Variscan shearing of high-grade metamorphic Moldanubian rocks. The shearing was associated with widespread chloritisation of biotite and formation of white mica. Chloritized zones were later intruded by saline, oxidized brines, capable of dissolving U from host rocks.
Related projects:	Conceptual model for uranium mineralization at the Rožná deposit Geological Processes and their Environmental Impact - Contact of the Variscides and Alpides