NONAUTONOMOUS PHASES AS POTENTIAL SOURCES OF INCOMPATIBLE ELEMENTS

Tauson V.L.; Akimov V.V.; Lipko S.V.; Loginov B.A.

dc.contributor.author	Tauson V.L.
dc.contributor.author	Akimov V.V.
dc.contributor.author	Lipko S.V.
dc.contributor.author	Loginov B.A.
dc.date.accessioned	2024-11-02T11:07:50Z
dc.date.available	2024-11-02T11:07:50Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13522510
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 280-283
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46354
dc.description.abstract	The genesis of some deposits of noble and rare metals, which are extremely scarce in crustal and mantle rocks, attracts permanent interest of specialists in the field of ore formation. A new systematics of absorption of trace elements by real mineral crystals with participation of the so-called nonautonomous phases has been elaborated recently. By definition, the nonautonomous phases cannot exist independent of crystal surface in contrast to the common (autonomous) phases, which can be separated from the system without a change of their composition and structure and alteration of related phases.
dc.title	NONAUTONOMOUS PHASES AS POTENTIAL SOURCES OF INCOMPATIBLE ELEMENTS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020292