THE EFFECT OF WATER ON MANTLE PHASE TRANSITIONS

dc.contributor.author	Ohtani E.
dc.contributor.author	Litasov K.D.
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=40690412
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2006, 62, 62. С. 3, 397-420
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/44632
dc.description.abstract	Water has played an important role in the Earth’s evolution. The incorporation of water as hydroxyl into solid mineral phases or as coexisting hydrous fluids and melts affects the chemical and physical properties of crust and mantle constituents, i.e., it weakens rocks and minerals, reduces viscosity and strength of the materials, and depresses dramatically the melting temperature of silicate minerals
dc.title	THE EFFECT OF WATER ON MANTLE PHASE TRANSITIONS
dc.type	Статья
dc.identifier.doi	10.2138/rmg.2006.62.17

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