POLYFACIES MODE OF IGNEOUS ROCKS AND METEORITES

dc.contributor.author	Marakushev A.A.
dc.contributor.author	Zinovieva N.G.
dc.contributor.author	Granovsky L.B.
dc.date.accessioned	2024-11-02T11:07:39Z
dc.date.available	2024-11-02T11:07:39Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520523
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 434-437
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46318
dc.description.abstract	The polyfacies mode of rocks and meteorites is related to their formation in several stages, which strongly differ in PT conditions. The polyfacies mode appears in igneous rocks during crystallization of magma owing to decrease in lithostatic pressure (depth) at the following stages: primary magma chamber–intermediate magma chambers–final consolidation of magma in intrusions or volcanic effusions (low-pressure minerals and volcanic glass). In contrast, minerals transported from deep-seated chambers are represented by high-pressure abyssal modifications.
dc.title	POLYFACIES MODE OF IGNEOUS ROCKS AND METEORITES
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030196

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