IRON-FREE DIOPSIDE ROCK, A NEW KIND OF MINERAL RAW MATERIAL

dc.contributor.author	Reznitskiy L.Z.
dc.contributor.author	Vishnyakov V.N.
dc.contributor.author	Vasil'yev Y.P.
dc.contributor.author	Vereshchagin V.T.
dc.contributor.author	Alekseyev Y.A.
dc.date.accessioned	2020-04-13T10:51:01Z
dc.date.available	2020-04-13T10:51:01Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30967357
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 97-99
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16676
dc.description.abstract	We studied the possibility of using metamorphic diopside-rich and diopside-bearing rocks, virtually devoid of iron, titanium and alkali oxides, in various silicate technologies. Such rocks are widespread in the Precambrian in the region south of Lake Baikal. The quartz-diopside rocks studied are metamorphic analogs of siliceous, dolomitic and calcitic-dolomitic deposits.
dc.subject	Precambrian	en
dc.title	IRON-FREE DIOPSIDE ROCK, A NEW KIND OF MINERAL RAW MATERIAL
dc.type	Статья
dc.subject.age	Precambrian	en
dc.subject.age	Докембрий	ru

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