KINETICS OF THE ALBITE-SANIDINE TRANSFORMATION IN THE PRESENCE OR ABSENCE OF QUARTZ

dc.contributor.author	Alekseev V.G.
dc.contributor.author	Medvedeva L.S.
dc.date.accessioned	2024-11-09T08:38:19Z
dc.date.available	2024-11-09T08:38:19Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13528515
dc.identifier.citation	Geochemistry International, 2006, 44, 2, 202-204
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46437
dc.description.abstract	The experiments were conducted with fractions of low albite, intermediate sanidine, and α-quartz crushed to 50–100 μm. The fractions were repeatedly rinsed with water in an ultrasonic bath to remove dust particles. The specific surface of albite and sanidine measured by the BET method is 0.11 m2/g. We performed four experimental series with different amounts of minerals (in mg) per 1 ml 0.1 m KHCO3.
dc.subject	albite
dc.subject	sanidine
dc.title	KINETICS OF THE ALBITE-SANIDINE TRANSFORMATION IN THE PRESENCE OR ABSENCE OF QUARTZ
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906020108

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