NATURAL PHOSPHATE-SULFATE MELTS

dc.contributor.author	Naumov V.B.
dc.contributor.author	Solovova I.P.
dc.contributor.author	Kovalenko V.I.
dc.contributor.author	Turkov V.A.
dc.contributor.author	Malov V.S.
dc.contributor.author	Samoylov V.S.
dc.date.accessioned	2020-04-13T10:51:02Z
dc.date.available	2020-04-13T10:51:02Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30967462
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 300, 3, 95-97
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16686
dc.description.abstract	A study of the numerous primary microinclusions found in apatite crystals from the Mushugay-Khuduk carbonatite complex (Mongolia) established the presence of natural phosphate-sulfate melts and their basic characteristics. The crystals studied came from the Apatitovyy rare earth and apatite ore body with a stock-like form measuring approx. 30 × 70 m and traced down to 200 m in boreholes. It cuts across its host syenite-porphyry massif, and numerous schlieren-like segregations of apatite ore, as also veins of it are observed in the exocontacts of the syenite-porphyry. Additional aspects of the subject are discussed.
dc.title	NATURAL PHOSPHATE-SULFATE MELTS
dc.type	Статья

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