Liquidus isotherms and phase equilibria have been determined experimentally for a pseudo-ternary section of the form “MnO”–(CaO+MgO)–(SiO
2+Al
2O
3) with a fixed Al
2O
3/SiO
2 weight ratio of 0.17 and MgO/CaO weight ratio of 0.25 for temperatures in the range 1 393–1 673 K.
The primary phase fields found in the investigated section include manganosite (Mn, Mg, Ca)O; dicalcium silicate α-2(Ca, Mg, Mn)O·SiO
2; merwinite 3CaO·(Mg, Mn)O·2SiO
2; melilite [2CaO·(MgO, MnO, Al
2O
3)·2(SiO
2, Al
2O
3)]; wollastonite [(Ca, Mg, Mn)O·SiO
2]; diopside [(CaO, MgO, MnO, Al
2O
3)·SiO
2]; tridymite (SiO
2); rhodonite [(Mn, Mg, Ca)O·SiO
2]; anorthite (CaO·Al
2O
3·2SiO
2) and tephroite [2(Mn, Mg, Ca)O·SiO
2].
The liquidus temperatures and primary phase fields are significantly different to those in the ternary system “MnO”–CaO–SiO
2, but are close to those previously reported pseudo-ternary section “MnO”–(CaO+MgO)–(SiO
2+Al
2O
3) for Al
2O
3/SiO
2 weight ratio of 0.17 and MgO/CaO weight ratio of 0.17.
The partitioning of CaO, MgO and MnO between liquid and solid phases was measured using EPMA, and the extents of solid solutions for a range of bulk compositions and temperatures were characterised.
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