THERMOCHEMICAL STUDY OF NATURAL PHENGITE

dc.contributor.author	Ogorodova L.P.
dc.contributor.author	Kiseleva I.A.
dc.contributor.author	Mel'chakova L.V.
dc.contributor.author	Shuriga T.N.
dc.date.accessioned	2024-10-23T07:15:42Z
dc.date.available	2024-10-23T07:15:42Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13508555
dc.identifier.citation	Geochemistry International, 2006, 44, 2, 196-198
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46103
dc.description.abstract	Phengite, K(Mg,Fe)0.5Al1.5[Si3.5Al0.5O10](OH)2, is a dioctahedral mica intermediate between muscovite and aluminoceladonite in the nomenclature. Divalent cations, mainly Mg2+ and Fe2+, substitute for Al in the octahedral sites of phengite. Since the total number of octahedral cations in the mineral remains two per formula unit, the content of tetrahedrally coordinated aluminum also decreases.
dc.subject	phengite
dc.title	THERMOCHEMICAL STUDY OF NATURAL PHENGITE
dc.type	Статья
dc.identifier.doi	10.1134/S001670290602008X

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