FORMATION OF REACTION GARNETS DURING MELTING OF THE MGCO3-CACO3- NAALSIO4-SIO2 SYSTEM AT 7.0 GPA

Litvin Yu.A.; Litvin V.Yu.; Kadik A.A.; Zharikov V.A.

dc.contributor.author	Litvin Yu.A.
dc.contributor.author	Litvin V.Yu.
dc.contributor.author	Kadik A.A.
dc.contributor.author	Zharikov V.A.
dc.date.accessioned	2024-11-09T08:38:24Z
dc.date.available	2024-11-09T08:38:24Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13529620
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 41-45
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46453
dc.description.abstract	The formation and evolution of deep-seated carbonatite magmas under the PT conditions of diamond formation represent complex physicochemical processes that incorporate multicomponent silicate material of mantle peridotite, strongly compressed carbonate melts, and CO2 fluids, which possibly represent the products of multiphase plume differentiation. Mobile low-viscosity carbonatite magmas belong to the chemically active forms of deep-seated matter of the dynamic mantle. It has been suggested that the carbonatite magmas contribute to mantle metasomatism as “carbonatite fluids”.
dc.title	FORMATION OF REACTION GARNETS DURING MELTING OF THE MGCO3-CACO3- NAALSIO4-SIO2 SYSTEM AT 7.0 GPA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010119