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• W2312865056 endingPage "2042" @default.
• W2312865056 startingPage "2035" @default.
• W2312865056 abstract "We investigated the properties of Al-bearing SiO2 (with 4 or 6 wt% Al2O3) at pressures and temperatures corresponding to the lowermost mantle, using laser-heated diamond-anvil cell coupled with synchrotron-based in situ X-ray diffraction. The phase transition from CaCl2-structured to α-PbO2- structured (seifertite) polymorphs occurs between 113 and 119 GPa at 2500 K. The range of pressure where the two phases coexist is small. There is a slight decrease of the transition pressure with increasing Al-content. We propose a tentative phase diagram reporting the minerals composition as a function of pressure in the SiO2-Al2O3 system." @default.
• W2312865056 created "2016-06-24" @default.
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• W2312865056 date "2014-10-01" @default.
• W2312865056 modified "2023-10-16" @default.
• W2312865056 title "Phase diagram and P-V-T equation of state of Al-bearing seifertite at lowermost mantle conditions" @default.
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• W2312865056 doi "https://doi.org/10.2138/am-2014-4697" @default.
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