THE SPECIFIC CHARACTER OF EVOLUTION OF FLUID-SILICATE-METALLIC IMMISCIBILITY OF MELTS

dc.contributor.author	Marakushev A.A.
dc.contributor.author	Rimkevich V.S.
dc.contributor.author	Dem'yanova L.P.
dc.date.accessioned	2026-04-25T09:32:55Z
dc.date.issued	2007
dc.description.abstract	Immiscibility in natural melts (magmas), which is expressed either in layering of intrusions or in formation of a droplike texture, develops under the influence of fluids that considerably decrease the crystallization temperature. Rhythmic magmatic layering is provided by deviation from equilibrium during fast cooling, when the melt layers have no time to change their composition, enter to the field of immiscibility, and are subjected to further immiscibility.
dc.identifier	https://elibrary.ru/item.asp?id=15292218
dc.identifier.citation	Doklady Earth Sciences, 2007, 413, 1, 308-314
dc.identifier.doi	10.1134/S1028334X07020407
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/52615
dc.title	THE SPECIFIC CHARACTER OF EVOLUTION OF FLUID-SILICATE-METALLIC IMMISCIBILITY OF MELTS
dc.type	Статья

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