Experimental investigation and optimization of thermodynamic properties and phase diagrams in the systems CaO-SiO2, MgO-SiO2, CaMgSi2O6-SiO2 and CaMgSi2O6-Mg2SiO4 to 1•0 GPa

被引:36
作者
Hudon, P
Jung, IH
Baker, DR
机构
[1] McGill Univ, Dept Earth & Planetary Sci, Montreal, PQ H3A 2A7, Canada
[2] Ecole Polytech, Ctr Res Computat Thermochem, Montreal, PQ H3C 3A7, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
CaO-SiO2; CaMgSi2O6-Mg2SiO4; CaMgSi2O6-SiO2; experiments; MgO-SiO2;
D O I
10.1093/petrology/egi037
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Using experimental results at 1.0 GPa for the systems CaO-SiO2, MgO-SiO2, CaMgSi2O6-SiO2 and CaMgSi2O6-Mg2SiO4, and all the currently available phase equilibria and thermodynamic data at 1 bar, we have optimized the thermodynamic properties of the liquid phase at 1.0 GPa. The new optimized thermodynamic parameters indicate that pressure has little effect on the topology of the CaO-SiO2, CaMgSi2O6-SiO2, and CaMgSi2O6-Mg2SiO4 systems but a pronounced one on the MgO-SiO2 binary. The most striking change concerns passage of the MgSiO3 phase from peritectic melting at 1 bar to eutectic melting at 1.0 GPa. This transition is estimated to occur at 0.41 GPa. For the CaMgSi2O6-SiO2 and CaMgSi2O6-Mg2SiO4 pseudo-binaries, the size of the field clinopyroxene + liquid increases with increasing pressure. This change is related to the shift of the piercing points clinopyroxene + silica + liquid (from 0.375 mol fraction SiO2 at 1 bar to 0.414 at 1.0 GPa) and clinopyroxene + olivine + liquid (from 0.191 mol fraction SiO2 at 1 bar to 0.331 at 1.0 GPa) that bound the clinopyroxene + liquid field in the CaMgSi2O6.SiO2 and CaMgSi2O6.Mg2SiO4 pseudo-binaries, respectively.
引用
收藏
页码:1859 / 1880
页数:22
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