首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Correction to 'Unified analyses for P-V-T equation of state of MgO: A solution for pressure-scale problems in high P-T experiments'
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Correction to 'Unified analyses for P-V-T equation of state of MgO: A solution for pressure-scale problems in high P-T experiments'

机译:对“ MgO的P-V-T状态方程的统一分析:高P-T实验中压力规模问题的解决方案”的更正

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In the paper "Unified analyses for P-V-T equation of state of MgO: A solution for pressure-scale problems in high P-T experiments" by Yoshinori Tange, Yu Nishihara, and Taku Tsuchiya (Journal of Geophysical Research, 114, B03208, doi:10.1029/2008JB005813, 2009), a postspinel phase boundary in Mg2SiO4 [Fei et al., 20046] and a postperovskite boundary in MgSiO3 [Hirose et al., 2006] were reassessed by using a P-V-T EOS of MgO proposed in this study based on the Scale-Free Unified Analysis (SFUA). However, we found that in Figure 11, the postperovskite boundary by Tsuchiya et al. [2004] was plotted incorrectly. Here the corrected Figure 11 is represented.
机译:Yoshinori Tange,Yu Nishihara和Taku Tsuchiya在论文“ MgO的PVT状态方程的统一分析:高PT实验中压力规模问题的解决方案”中(地球物理研究杂志,114,B03208,doi:10.1029 / (2008JB005813,2009),使用MgO的PVT EOS,根据规模,重新评估了Mg2SiO4中的松石后相边界[Fei等,20046]和钙钛矿后的钙钛矿后边界[Hirose等,2006]。 -免费的统一分析(SFUA)。然而,我们发现在图11中,Tsuchiya等人的钙钛矿后边界。 [2004]被错误地绘制。此处显示了校正后的图11。

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