REDOX STATE OF ECLOGITES AND PERIDOTITES FROM SUB-CRATONIC UPPER MANTLE AND A CONNECTION WITH DIAMOND GENESIS

dc.contributor.author	Simakov S.K.
dc.date.accessioned	2024-07-14T10:19:07Z
dc.date.available	2024-07-14T10:19:07Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=13509597
dc.identifier.citation	Contributions to Mineralogy and Petrology, 2006, 151, 3, 282-296
dc.identifier.issn	0010-7999
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/44429
dc.description.abstract	Pressure-Temperature- fO2 conditions and fluid compositions estimated for mineral parageneses from inclusions in diamonds, diamond-bearing and diamond-free xenoliths using a garnet-clinopyroxene-silica oxygen barometer data indicate that the upper mantle is zoned, with a relatively oxidized lithosphere and a reduced asthenosphere. Calculations in the C-O-H system indicate that eclogite inclusions within diamonds and xenoliths have formed mainly in equilibrium with water-rich fluids. © Springer-Verlag 2006.
dc.subject	BAROMETRY
dc.subject	DIAMOND GENESIS
dc.subject	MANTLE
dc.subject	OXYGEN FUGACITY
dc.title	REDOX STATE OF ECLOGITES AND PERIDOTITES FROM SUB-CRATONIC UPPER MANTLE AND A CONNECTION WITH DIAMOND GENESIS
dc.type	Статья
dc.identifier.doi	10.1007/s00410-005-0058-z

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