REAL STRUCTURE AND PHYSICAL PROPERTIES OF CHROMITES AS AN INDICATOR OF THEIR GENESIS

dc.contributor.author	Svetov S.A.
dc.contributor.author	Kevlich V.I.
dc.contributor.author	Fofanov A.D.
dc.contributor.author	Repnikova E.A.
dc.contributor.author	Smol'kin V.F.
dc.contributor.author	Moshkina E.V.
dc.date.accessioned	2022-01-15T07:43:06Z
dc.date.available	2022-01-15T07:43:06Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13440574
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 9, 1272-1275
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34331
dc.description.abstract	Spinels (Mg,Fe2+)(Cr,Al,Fe3+)2O4 are the most informative minerals for reconstruction of PT crystallization parameters and differentiation conditions of ultramaﬁc melts [1]. It is known that the real structure and physical properties of spinels are governed by their formation conditions (chemical composition of the melt, temperature and pressure of crystallization, and others) [2, 3].
dc.title	REAL STRUCTURE AND PHYSICAL PROPERTIES OF CHROMITES AS AN INDICATOR OF THEIR GENESIS
dc.type	Статья

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