FIRST DIAMOND FINDS IN PLUTONIC XENOLITHS AT THE EASTERN MARGIN OF THE SIBERIAN CRATON

dc.contributor.author	Biryukov V.M.
dc.contributor.author	Gernov P.Y.
dc.contributor.author	Ivanov G.I.
dc.contributor.author	Kosygin Y.A.
dc.date.accessioned	2020-10-02T08:47:03Z
dc.date.available	2020-10-02T08:47:03Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31074331
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1989, 305, 2, 122-125
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17633
dc.description.abstract	Numerous diamond finds in nonkimberlitic, basaltoid and ultramafic rocks and their serpentinized varieties, commonly with pyrope garnet, as well as in lamproites and mineralogically different types of eclogite, have greatly broadened our ideas about the physical conditions of natural diamond synthesis. Especially informative in this respect are plutonic xenoliths in some types of alkanic basalt and kimberlite breccia, as well as solid inclusions of one or more minerals in diamond crystals. Our diamond finds in plutonic xenoliths of eclogitic rock from compositionally unique kimberlite breccia now add to what is already known about those conditions.
dc.title	FIRST DIAMOND FINDS IN PLUTONIC XENOLITHS AT THE EASTERN MARGIN OF THE SIBERIAN CRATON
dc.type	Статья

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