THE PARTITIONING OF WATER BETWEEN NOMINALLY ANHYDROUS MINERALS AND SILICATE MELTS

dc.contributor.author	Kohn S.C.
dc.contributor.author	Grant K.J.
dc.date.accessioned	2025-03-29T04:40:20Z
dc.date.available	2025-03-29T04:40:20Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=13736835
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2006, 62, 62. С. 2, 231-241
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/48656
dc.description.abstract	Many chapters in this volume emphasize that water plays a crucial role in determining the properties and behavior of the mantle. One of the most important examples of the effect of water on mantle behavior is its dramatic effect in reducing melting temperatures, and, in the case of decompression melting, increasing the depth of initiation of melting. Even the small amount of water which could be contained within nominally anhydrous minerals (NAMs) is sufficient to play an important role in generation of MORBs.
dc.title	THE PARTITIONING OF WATER BETWEEN NOMINALLY ANHYDROUS MINERALS AND SILICATE MELTS
dc.type	Статья
dc.identifier.doi	10.2138/rmg.2006.62.10

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