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- W1996163598 abstract "Abstract The following geochemical rules-of-thumb seem to hold for vanadium: 1. (1) Magnetites as a group have higher V contents than either hematites or ilmenites. 2. (2) In magnetite—hematite pairs, however, the hematite has the higher V content. 3. (3) In magnetite—ilmenite pairs, the magnetite is usually richer in V than the ilmenite, although the enrichment factor is highly variable, between 1 and 20, and in one particular case even clearly 4. (4) In hematite—rutile pairs, the rutile strongly concentrates V. This behaviour of V is understandable from the interplay of two simple considerations, namely: (a) under most conditions in which magnetite and/or ilmenite are stable at high temperatures V is dominantly three-valent, and substitutes mainly for Fe 3+ ; and (b) when the oxygen fugacity is close to that defined by the magnetite—hematite equilibrium, V changes to valency 4+, and proxies mostly for Ti 4+ , in hemo-ilmenites, ilmenohematites, or rutile." @default.
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- W1996163598 date "1980-08-01" @default.
- W1996163598 modified "2023-10-16" @default.
- W1996163598 title "Geochemical behaviour of vanadium in iron—titanium oxides" @default.
- W1996163598 cites W1973544042 @default.
- W1996163598 doi "https://doi.org/10.1016/0009-2541(80)90121-7" @default.
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