Nová Ves u Rýmařova – ložisko olověno-zinkových rudČlánek v PDF
Nová Ves near Rýmařov – Pb-Zn ore deposit (Jeseníky Mts., Czech Republic)
Seven veins, a few veinlets and disseminated accumulations form the ore body in metamorphosed Devonian vulcanosediments near the village Nová Ves (Jeseníky Mts.). There were distinguished two mineralization stages with repetition of common sulfides and carbonates as gangue minerals.
The analyses of the fluid inclusions in sphalerite indicate the low salinity of chloride solutions. Calculated sulfur isotopic temperatures of sulfide crystallization (from 55 to 360 ºC) correspond to two mineralization stages. Sulfur in ore-bearing fluids was probably derived from the deep-seated sources. The thermodynamic modeling suggests that the sulfur fugacity change log aS2 from -4 to -17 was the main factor of the ore formation.
Bohuslav Fojt, Josef Zeman, Department of Geological Sciences, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic
František Čermák, Jesenická 17, 795 01 Rýmařov, Czech Republic
Jana Ďurišová, Jana Hladíková, Czech Geological Service, Geologická 6, 152 00 Praha 5 – Barrandov, Czech Republic
Vladimír Hoffman, Zdeněk Trdlička, Department of the Raw Materials, Vítězná 425, 284 03 Kutná Hora, Czech Republic
Dušan Kopa, Silesian Museum, Tyršova I, 746 46 Opava, Czech Republic