Crystal structure, Raman and FTIR spectroscopy, and equations of state of OH-bearing MgSi[O.sub.3] akimotoite
MgSi[O.sub.3] akimotoite is stable relative to majoritegarnet under low-temperature geotherms within steeply or rapidly subducting slabs. Two compositions of Mg-akimotoite were synthesized under similar conditions: Z674 (containing about 550 ppm wt [H.sub.2]O) was synthesized at 22 GPa and 1,500°C a...
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Veröffentlicht in: | Contributions to mineralogy and petrology 2013-11, Vol.166 (5), p.1375 |
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Sprache: | eng |
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