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.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.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.doi | 10.2138/rmg.2006.62.7 | |
| dc.identifier.issn | 1529-6466 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/48458 | |
| dc.title | WATER IN NATURAL MANTLE MINERALS I: PYROXENES | |
| dc.type | Статья |
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