CHEMICAL COMPOSITION OF MAGMA (MELT INCLUSIONS) OF MELILITE-BEARING NEPHELINITE FROM THE BELAYA ZIMA CARBONATITE COMPLEX, EASTERN SAYAN

dc.contributor.author	Andreeva I.A.
dc.contributor.author	Kovalenko V.I.
dc.contributor.author	Kononkova N.N.
dc.date.accessioned	2022-07-18T05:29:15Z
dc.date.available	2022-07-18T05:29:15Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13451886
dc.identifier.citation	Doklady Earth Sciences, 2004, 394, 1, 116-119
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38243
dc.description.abstract	The detailed investigation of melt inclusions in nepheline and perovskite showed that the rock formation proceeded from incompletely saturated with silica high-Ca magmatic melt substantially enriched with alkaline, rare and volatile components such as H 2O, CO 2, Cl and S. Established for the first time niobium-tantalum character of the parent for the studied rocks magmas definitely confirms the geochemical specificity of the Belaya Zima deposit.
dc.title	CHEMICAL COMPOSITION OF MAGMA (MELT INCLUSIONS) OF MELILITE-BEARING NEPHELINITE FROM THE BELAYA ZIMA CARBONATITE COMPLEX, EASTERN SAYAN
dc.type	Статья

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