ENDOGENE ORIGIN OF PERLITE, OBSIDIAN AND PUMICE (EXPERIMENTAL SIMULATION)

dc.contributor.author	Marakushev A.A.
dc.contributor.author	Persikov E.S.
dc.contributor.author	Bukhtiyarov P.G.
dc.date.accessioned	2020-10-09T08:55:40Z
dc.date.available	2020-10-09T08:55:40Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31122788
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 1, 131-135
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17840
dc.description.abstract	Our experimental simulation of the dehydration of silicic water-bearing melts, together in petrographic and physicochemical analysis of the natural features of silicic volcanic activity, confirms that silicic glasses of the obsidian-perlite-pumite series have a common origin. The formation of structural-textural varieties of these glasses, like the differences in their water content, result from the dynamic features of dehydration, decompression, vesiculation and cooling of intruded water-rich silicic magmas with special physicochemical properties.
dc.title	ENDOGENE ORIGIN OF PERLITE, OBSIDIAN AND PUMICE (EXPERIMENTAL SIMULATION)
dc.type	Статья

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