EVIDENCE OF THE EXISTENCE OF HIGH-ALUMINA CLINOPYROXENE (TSCHERMAKITE) IN GARNET PYROXENITES FROM THE KOKCHETAV MASSIF, KAZAKHSTAN

dc.contributor.author	Reverdatto V.V.
dc.contributor.author	Korolyuk V.N.
dc.contributor.author	Selyatitsky A.Yu.
dc.date.accessioned	2022-01-16T05:05:34Z
dc.date.available	2022-01-16T05:05:34Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13444830
dc.identifier.citation	Doklady Earth Sciences, 2003, 391, 6, 896-899
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34363
dc.description.abstract	Our study showed that anorthite-zoisite-spinel/magnetite-corundum pseudomorphs in coronites of the Kokchetav Massif developed after high-alumina clinopyroxene (tschermakite) (Ca,Fe,Mg Al2SiO6. This phase is stable only at high PT parameters. Therefore, it can be replaced by aggregate of later minerals during retrograde metamorphism.
dc.subject	Tschermakite
dc.title	EVIDENCE OF THE EXISTENCE OF HIGH-ALUMINA CLINOPYROXENE (TSCHERMAKITE) IN GARNET PYROXENITES FROM THE KOKCHETAV MASSIF, KAZAKHSTAN
dc.type	Статья

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