DIAMONDIFEROUS XENOLITHS AND MEGACRYSTS FROM THE NYURBINSKAYA KIMBERLITE PIPE (NAKYNSKY FIELD, YAKUTIA)

dc.contributor.author	Spetsius Z.V.
dc.contributor.author	Ivanov A.S.
dc.contributor.author	Mityukhin S.I.
dc.date.accessioned	2024-10-23T07:15:44Z
dc.date.available	2024-10-23T07:15:44Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13509024
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 779-783
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46109
dc.description.abstract	Paragenetic associations with diamond in kimberlites can be subdivided into three main types: (1) inclusions of various minerals in diamond crystals, (2) mineral intergrowths with diamonds, and (3) xenoliths of diamondiferous mantle rocks. These types are found in different proportions in all the kimberlite pipes with commercial diamond contents. Such rocks have always attracted attention of researchers, since they bear the most reliable information on natural formation environments of diamonds and their peculiarities, i.e., petrological features of the upper mantle in the region.
dc.subject	diamond
dc.subject	Nyurbinskaya kimberlite pipe
dc.title	DIAMONDIFEROUS XENOLITHS AND MEGACRYSTS FROM THE NYURBINSKAYA KIMBERLITE PIPE (NAKYNSKY FIELD, YAKUTIA)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050230

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