2009
DOI: 10.1016/j.gca.2009.02.033
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The crystal and melt structure of spinel and alumina at high temperature: An in-situ XANES study at the Al and Mg K-edge

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Cited by 46 publications
(34 citation statements)
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“…It is well known that Mg 2+ element forms a very stable spinel with alumina and that it is not possible to quench this MgAl 2 O 4 composition or other magnesium aluminate compositions using fast quench. This crystalline phase shows that Mg and Al are in 4 and 6 fold coordination respectively at room temperature and shows an inversion of the site with temperature [20][21][22]. In SrO-Al 2 O 3 and BaO-Al 2 O 3 systems, the melting temperatures are higher than in the CaO-Al 2 O 3 system in agreement with those determined in the alkaline-earth aluminosilicate systems, which increase with the size of alkaline-earth cation [23].…”
Section: Introductionsupporting
confidence: 76%
“…It is well known that Mg 2+ element forms a very stable spinel with alumina and that it is not possible to quench this MgAl 2 O 4 composition or other magnesium aluminate compositions using fast quench. This crystalline phase shows that Mg and Al are in 4 and 6 fold coordination respectively at room temperature and shows an inversion of the site with temperature [20][21][22]. In SrO-Al 2 O 3 and BaO-Al 2 O 3 systems, the melting temperatures are higher than in the CaO-Al 2 O 3 system in agreement with those determined in the alkaline-earth aluminosilicate systems, which increase with the size of alkaline-earth cation [23].…”
Section: Introductionsupporting
confidence: 76%
“…The first spinel peak is 1567 eV (Neuville et al. ); the first corundum peak (also CN = 6) is at 1568 ± 0.6 eV (Li et al. ; Ildefonse et al.…”
Section: Results and Discussion Ii: Analyses Of Three Tracks Of Probamentioning
confidence: 99%
“…The lower 1565 eV peak corresponds to four-fold symmetry and could be due to transfer to CN = 4 in high-temperature inverted spinel or Al-rich spinel (Neuville et al 2009); or it could be due to an admixture of CN = 4 aluminosilicate, for example, we show oligoclase (80% albite, 20% anorthite) in Fig. 11.…”
Section: Stxm1 Characterization Of Orionmentioning
confidence: 88%
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