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