PETROCHEMICAL AND MINERALOGICAL CONSTRAINTS FOR DIAGNOSTICS OF YAKUTIAN KIMBERLITES

dc.contributor.author	Golubeva Yu.Yu.
dc.contributor.author	Tsepin A.I.
dc.date.accessioned	2022-08-03T05:21:01Z
dc.date.available	2022-08-03T05:21:01Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13466395
dc.identifier.citation	Doklady Earth Sciences, 2004, 397, 6, 798-803
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38469
dc.description.abstract	Typomorphic minerals were studied in order to refine the nomenclature of alkaline ultramafic rocks. These are micas and perovskites. We compared chemical compositions of micas from typical kimberlites, such as the Udachnaya pipe (Daldyn field), Malyi Kounamka pipe (Kuranakh field), Nebaibyt pipe )Srednii Kounamka field), and Bazovaya 2 and Billyakh 4 pipes (Kharamai field), with those from aforementioned objects, which, geochemically, approximate orangeites and lamproites.
dc.title	PETROCHEMICAL AND MINERALOGICAL CONSTRAINTS FOR DIAGNOSTICS OF YAKUTIAN KIMBERLITES
dc.type	Статья

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