Fluid inclusions, stable isotopes and mineralogical constraints on the genesis of Roudný gold-deposit, Czech Republic.

Abstract

The early mineralization stages occurred from H2O-CO2 low salinity, high-T (~ 350 to 300 °C) metamorphic fluids; the younger stages from H2O-only fluids (~250°C and 8 ? 9 wt. % NaCl eqv. to ~120°C and 6 - 7 wt. % NaCl eqv.).

Keywords

• Jiří Zachariáš
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