FINELY DIVIDED SILVER IN SILICIC VOLCANICS

dc.contributor.author	Lobanov A.S.
dc.date.accessioned	2020-04-08T08:52:36Z
dc.date.available	2020-04-08T08:52:36Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30935862
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 145-147
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16385
dc.description.abstract	Finely divided native silver was detected among rock-forming silicates in silicic volcanics hosting a lead-zinc deposit in Soviet Central Asia. It is scattered through the rock as particles both visible and indistinguishable under the optical microscope and appears not only in, but also outside of the zone of commercial ore mineralization. Taking into account our data, we may assume that finely divided silver is widespread in volcanic host rocks of stockwork-type silver and lead-zinc deposits and could be both a source and an indicator of economic silver concentrations.
dc.title	FINELY DIVIDED SILVER IN SILICIC VOLCANICS
dc.type	Статья

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