WATER IN NATURAL MANTLE MINERALS II: OLIVINE, GARNET AND ACCESSORY MINERALS

dc.contributor.author	Beran A.
dc.contributor.author	Libowitzky E.
dc.date.accessioned	2024-08-03T06:11:01Z
dc.date.available	2024-08-03T06:11:01Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=38921119
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2006, 62, 62. С. 1, 169-192
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/44631
dc.description.abstract	Hydrogen traces change the physical properties of mantle minerals to an extent that is far out of proportion to its low concentration. These properties include mechanical strength, melting behavior, diffusion rate, electrical conductivity, viscosity and rheology. Besides minerals of the pyroxene group, the close-packed mineral structures of olivine, garnet and some accessory minerals offer important storage sites for hydrogen traces in the Earth’s mantle.
dc.title	WATER IN NATURAL MANTLE MINERALS II: OLIVINE, GARNET AND ACCESSORY MINERALS
dc.type	Статья
dc.identifier.doi	10.2138/rmg.2006.62.8

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