The Journal of Geology · 1950 · 158 citations · 4 references
Natural SciencesEarth SciencesMaterials ScienceCrystal StructurePhysical ChemistrySolidificationCrystallization ProcessesPartial MeltingSilicate MineralsCrystal-melt EquilibriumFeldspar MineralsFeldspar PetrologyMelting RelationsMineral-melt EquilibriumPressure Dependence Of MeltingSilicate Phase Equilibria
A study, of the alkali-feldspar join $$KAlSi_{3}O_{8}-NaAlSi_{3}O_{8}$$ in the system $$NaAlSiO_{4}-KAlSiO_{4}-SiO_{2}$$ shows an unbroken series of solid solutions between these alkali feldspars with a minimum on the melting and freezing curves at $$1,063^{\circ} \pm 3^{\circ} C$$. at 35 weight per cent potash feldspar. All alkali-feldspar compositions with more than 49 weight per cent potash feldspar melt incongruently and have leucite crystals present, which disappear only at higher temperatures. A revised equilibrium diagram for the system $$NaAlSiO_{4}-KAlSiO_{4}-SiO_{2}$$ is given; the data on which it is based will be published in full later.
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High-Temperature Albite and Contiguous Feldspars
O. F. Tuttle, N. L. Bowen · The Journal of Geology · 1950 · 102 citations
The melting of potash feldspar
G. W. Morey, N. L. Bowen · American Journal of Science · 1922 · 26 citations · Full text