Silver minerals from Rudabánya (N-Hungary)
Numerous silver minerals were found recently in the primary and in the secondary oxidation zone of the hydrothermal-metasomatic iron ore deposit at RudabSnya, Northern-Hungary. In the baritized zone bound to the carbonatic ore - primary in the galena-rich orebodies - silver, acanthite, proustite, py...
Elmentve itt :
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Dokumentumtípus: | Cikk |
Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1995
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Sorozat: | Acta mineralogica-petrographica
36 |
Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
Tárgyszavak: | |
Online Access: | http://acta.bibl.u-szeged.hu/24820 |
Tartalmi kivonat: | Numerous silver minerals were found recently in the primary and in the secondary oxidation zone of the hydrothermal-metasomatic iron ore deposit at RudabSnya, Northern-Hungary. In the baritized zone bound to the carbonatic ore - primary in the galena-rich orebodies - silver, acanthite, proustite, pyrargyrite and xanthoconite? were found. The limonitic and siliceous limonitic ores of the oxidation zone contains acanthite, moschellandsbergite, bromargyrite, chlorargyrite and iodargyrite. These minerals are the resultant products of the recrystallization of the silver-bearing phases of the baritized zone, i.e. of secondary origin. This paper is on the description of the minerals referred to above. |
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Terjedelem/Fizikai jellemzők: | 5-15 |
ISSN: | 0365-8066 |