Comparative Study of Bi-Te-Se-S Mineralizations in Slovak Republic and Transcarpathian Region of Ukraine. Part 1. Localities, Geological Situation and Mineral Associations

Comparative analysis of telluride occurrences found in the territory of Slovakia and Transcarpathians (Ukraine) has shown that there is distinct difference between the mode of Au-Ag-Bi-Te-Se mineralization of these regions. But within the area of distribution of neovolcanites Bi-Te-Se-S mineralizati...

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Збережено в:
Бібліографічні деталі
Дата:2009
Автори: Melnikov, V., Jelen, S., Bondarenko, S., Balintova, T., Ozdin, D., Grinchenko, A.
Формат: Стаття
Мова:English
Опубліковано: Інститут геохімії, мінералогії та рудоутворення ім. М.П. Семененка НАН України 2009
Назва видання:Мінералогічний журнал
Теми:
Онлайн доступ:http://dspace.nbuv.gov.ua/handle/123456789/30918
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Назва журналу:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Цитувати:Comparative Study of Bi-Te-Se-S Mineralizations in Slovak Republic and Transcarpathian Region of Ukraine. Part 1. Localities, Geological Situation and Mineral Associations / V. Melnikov, S. Jelen, S. Bondarenko, T. Balintova, D. Ozdin, A. Grinchenko // Мінералогічний журнал. — 2009. — Т. 31, № 4. — С. 38-48. — Бібліогр.: 38 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine
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Резюме:Comparative analysis of telluride occurrences found in the territory of Slovakia and Transcarpathians (Ukraine) has shown that there is distinct difference between the mode of Au-Ag-Bi-Te-Se mineralization of these regions. But within the area of distribution of neovolcanites Bi-Te-Se-S mineralization is generally represented by similar mineralogical phases. In the Transcarpathian region bismuth tellurides (tsumoite, pilsenite, joseites, native bismuth and poorly studied sulpho-selenotellurides of bismuth) were found only in metasomatites as secondary quartzites of the Vyghorlat-Guta ridge area. (Il'kivtsy, Podulky, Smerekiv Kamin'). The similar mineralization have been also found in some neovolcanites of Slovakia (Poruba pod Vigorlatom, Remetska Hamra).