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RMS Annual Session combined with the Fedorov Session 2014
Saint Petersburg, Russia
7-9 October 2014
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Vein alunite from the barite-quartz hydrothermal veins of the Beregovo mine field

RMS-DPI code:  2014-1-48-0
Scientific session:  M2. Mineralogy and geochemistry of precious metals
Author listing:  Slovotenko N.A., Skakun L.Z., Serkiz R.Ya.
Principal author:  Slovotenko Nadiya Alexandrovna
Language:  Russian
Abstract - Summary 
(short description):
Beregivske ore field is located in the Transcarpathian region of Ukraine, it is localized at the junction of the Transcarpathian volcanic belt of the Carpathians and the Pannonian median mass. Hydrothermal deposits of ore field belong to the epithermal type and presented by noble metal and polymetallic ore. Rare finding of alunite in the lower horizons in barite-quartz veins caught our attention, and we have attempted to identify the reasons for its occurrence. The main research tool was selected ontogenetic and cathodoluminescence methods of the mineralogy. As a result, it is determined that the alunite arose later than barite. The alunite appearance was possible by a greater flow of acid solutions in the mineral forming system.
Key words: epithermal, alunite, barite, cathodoluminescence.
 
RMS-DPI code:  2014-1-48-0
File of proceedings 
(PDF): 
 1178 K
Status:  printed
Recieved:  08/07/2014
Accepted:  31/08/2014
Published on-line:  28/12/2015
Permanent address of publication:  http://www.minsoc.ru/2014-1-48-0/
Contact author(s):  Slovotenko, Nadiya Alexandrovna
 

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