A SHORT OUTLINE OF THE TUNNEL OXIDES

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dc.contributor.author Pasero M.
dc.date.accessioned 2023-12-30T07:21:43Z
dc.date.available 2023-12-30T07:21:43Z
dc.date.issued 2005
dc.identifier https://www.elibrary.ru/item.asp?id=31378737
dc.identifier.citation Reviews in Mineralogy and Geochemistry, 2005, 57, С. 2, 291-305
dc.identifier.issn 1529-6466
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/42407
dc.description.abstract Within the large and comprehensive group of oxide minerals, the most relevant subgroup in the frame of microporous materials is that of the so-called “tunnel oxides.” This rather generic term historically refers to a number of minerals which, from a chemical point of view, are (mainly) manganese oxides. In nature manganese occurs in three different oxidation states—Mn2+, Mn3+ and Mn4+—with the latter being the dominant form in tunnel oxides.
dc.subject tunnel oxides
dc.title A SHORT OUTLINE OF THE TUNNEL OXIDES
dc.type Статья
dc.identifier.doi 10.2138/rmg.2005.57.9


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