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Evolution of ore-forming fluids along the Rožná-Olší shear zone, Bohemian Massif, Czech Republic: Implications for local uranium deposition and comparison with U-mineralization at Schlema, Erzgebirge, Germany
- 1.0207849 - USMH-B 20020285 RIV CZ eng C - Conference Paper (international conference)
Hein, U. - Lehman, B. - Kříbek, B. - René, Miloš
Evolution of ore-forming fluids along the Rožná-Olší shear zone, Bohemian Massif, Czech Republic: Implications for local uranium deposition and comparison with U-mineralization at Schlema, Erzgebirge, Germany.
Uranium deposits: From their genesis to their environmental aspects. Praha: Český geologický ústav, 2002 - (Kříbek, B.; Zeman, J.), s. 61-64. ISBN 80-7075-583-0.
[Uranium deposits: From their genesis to their environmental aspects. Praha (CZ), 10.09.2002-11.09.2002]
R&D Projects: GA ČR GA205/00/0212
Institutional research plan: CEZ:AV0Z3046908
Keywords : ore fluids * uranium
Subject RIV: DB - Geology ; Mineralogy
The late-Variscan primary uranium mineralization was precipitated from low-salinity aqueous solutions at epithermal conditions. The overall temporal evolution of the ore forming fluids is identical with that of polymetallic vein-type systems in large parts of Western and Central Europe.
Permanent Link: http://hdl.handle.net/11104/0103413
Number of the records: 1