WATER IN NATURAL MANTLE MINERALS I: PYROXENES

dc.contributor.author	Skogby H.
dc.date.accessioned	2025-03-15T04:58:30Z
dc.date.available	2025-03-15T04:58:30Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=28029619
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2006, 62, 62. С. 1, 155-167
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/48458
dc.description.abstract	A large number of studies of water in pyroxenes have confirmed that essentially all pyroxenes of terrestrial origin as a rule contain substantial amounts of OH, varying as a function of chemical composition and geological occurrence. The highest OH-concentrations are observed in mantle-derived samples, and it is now well established that both clino- and orthopyroxene can be considered as major host minerals for water in the mantle.
dc.title	WATER IN NATURAL MANTLE MINERALS I: PYROXENES
dc.type	Статья
dc.identifier.doi	10.2138/rmg.2006.62.7

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