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...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: Szakáll Sándor
Kovács Árpád
Dokumentumtípus: Cikk
Megjelent: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1995
Sorozat:Acta mineralogica-petrographica 36
Kulcsszavak:Kőzettan, Ásványtan, Földtan
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24820
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490 0 |a Acta mineralogica-petrographica  |v 36 
520 3 |a 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. 
650 4 |a Természettudományok 
650 4 |a Föld- és kapcsolódó környezettudományok 
695 |a Kőzettan, Ásványtan, Földtan 
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856 4 0 |u http://acta.bibl.u-szeged.hu/24820/1/mineralogica_036_005-015.pdf  |z Dokumentum-elérés