PICROILMENITE FROM KIMBERLITES OF THE DALDYN FIELD, YAKUTIA

dc.contributor.author	Alymova N.V.
dc.contributor.author	Kostrovitskii S.I.
dc.contributor.author	Ivanov A.S.
dc.contributor.author	Serov V.P.
dc.date.accessioned	2022-07-18T05:29:17Z
dc.date.available	2022-07-18T05:29:17Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13453910
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 3, 444-447
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38263
dc.description.abstract	The compositional structure of kimberlite fields is among the blank spots in the geology of kimberlite volcanism. Identification of pipe clusters within a kimberlite field is based on the geographic principle only, i.e., the spaial association of kimberlite bodies. We used one of the typomorphic kimberlite minerals-picroilmenite in-order to analyze the kibmberlite field structure. The abundance of picroilmenite, its stability during the hypergene disintegration of kimberlites and the formation of diamond collectors, and other specific features define a major role or this mineral in prospecting work.
dc.title	PICROILMENITE FROM KIMBERLITES OF THE DALDYN FIELD, YAKUTIA
dc.type	Статья

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