PETROCHEMICAL AND MINERALOGICAL CONSTRAINTS FOR DIAGNOSTICS OF YAKUTIAN KIMBERLITES

dc.contributor.authorGolubeva Yu.Yu.
dc.contributor.authorTsepin A.I.
dc.date.accessioned2022-08-03T05:21:01Z
dc.date.available2022-08-03T05:21:01Z
dc.date.issued2004
dc.description.abstractTypomorphic 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.identifierhttps://www.elibrary.ru/item.asp?id=13466395
dc.identifier.citationDoklady Earth Sciences, 2004, 397, 6, 798-803
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38469
dc.titlePETROCHEMICAL AND MINERALOGICAL CONSTRAINTS FOR DIAGNOSTICS OF YAKUTIAN KIMBERLITES
dc.typeСтатья

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