CHROMIUM SCHREYERITE AND CHROMIUM-VANADIUM-MANGANESE-IRON-ZINC SPINEL IN QUARTZITIC SILLIMANITE-CORDIERITE SCHISTS OF THE OLKHON AREA SOUTHWEST OF LAKE BAIKAL

dc.contributor.author	Boronikhin V.A.
dc.contributor.author	Dmitriyeva M.T.
dc.contributor.author	Koneva A.A.
dc.contributor.author	Korikovskiy S.P.
dc.date.accessioned	2020-11-02T00:30:42Z
dc.date.available	2020-11-02T00:30:42Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31129444
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 5, 176-180
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18343
dc.description.abstract	New vanadium minerals recently discovered in metamorphic rocks and pyrite ores include schreyerite, V2Ti3O9, and vuorelainenite (Mn, Fe)V2O4, the end member of the chromium-vanadium manganospinel series. We succeeded in finding both these coexisting minerals in high-alumina schists of the Ol'khon area. Our schreyerite is a hitherto unknown high-chromium variety, but the spinel is the variety intermediate between vuorelainenite (sic) and manganochromite. This paper discusses the mineralogy of these finds.
dc.title	CHROMIUM SCHREYERITE AND CHROMIUM-VANADIUM-MANGANESE-IRON-ZINC SPINEL IN QUARTZITIC SILLIMANITE-CORDIERITE SCHISTS OF THE OLKHON AREA SOUTHWEST OF LAKE BAIKAL
dc.type	Статья

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