| Reference Type | Journal (article/letter/editorial) |
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| Title | Synthetic armalcolite and pseudobrookite |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Medvedev, A. Ya. | Author |
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| Year | 1996 (April) | Volume | 60 |
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| Page(s) | 347-353 | Issue | 399 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_60/60-399-347.pdf+ |
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| DOI | doi:10.1180/minmag.1996.060.399.09Search in ResearchGate |
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| Mindat Ref. ID | 33 | Long-form Identifier | mindat:1:5:33:2 |
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| GUID | c9008a12-f917-43c8-a99e-054629b3f219 |
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| Full Reference | Medvedev, A. Ya. (1996) Synthetic armalcolite and pseudobrookite. Mineralogical Magazine, 60 (399) 347-353 doi:10.1180/minmag.1996.060.399.09 |
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| Plain Text | Medvedev, A. Ya. (1996) Synthetic armalcolite and pseudobrookite. Mineralogical Magazine, 60 (399) 347-353 doi:10.1180/minmag.1996.060.399.09 |
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| In | (1996, April) Mineralogical Magazine Vol. 60 (399) Mineralogical Society |
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| Abstract/Notes | AbstractArmalcolite and pseudobrookite have been crystallized from synthetic melts of basaltic composition with variable amounts of added TiO2. It was found that the composition of the armalcolite and pseudobrookite are dependent on the TiO2 content of the melt and the conditions (particularly oxygen fugacity, but also temperature and quenching rate) of formation. The maximum Al2O3 content of pseudobrookite appears to be ∼14–15 wt.% Al2O3, a spinel-like phase being exsolved at higher Al2O3 concentrations. Generally armalcolite is formed at low pO2 and pseudobrookite at higher oxygen fugacities. |
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These are possibly similar items as determined by title/reference text matching only.
