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Anorthite, a feldspar mineral, calcium aluminosilicate (CaAl2Si2O8), that occurs as white or grayish, brittle, glassy crystals.
Chabazite, common hydrated sodium and calcium aluminosilicate mineral, (Ca,Na2 Al2Si4O12·6H2O, in the zeolite family.
Epistilbite, hydrated sodium and calcium aluminosilicate mineral in the zeolite family.
Faujasite, hydrated sodium and calcium aluminosilicate mineral that is a rare member of the zeolite family.
Mordenite, hydrated sodium, potassium, and calcium aluminosilicate mineral (Na2,K2,Ca) Al2Sin0O24·7H2O, in the zeolite family.
Wairakite, hydrated calcium aluminosilicate mineral present in hot-spring deposits, notably those at Wairakei, New Zealand, and Onikobe, Japan.
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The basis of glass phase is calcium aluminosilicates.
The feldspathoid group minerals are sodium, potassium, and calcium aluminosilicates, many of which resemble the feldspars in appearance.
High-temperature eutectics (1473 1673 K) on the base of calcium aluminosilicates are represented as a matrix material.
The feldspar minerals are mixtures of sodium, potassium, and calcium aluminosilicates, and any feldspar may be classed by its percentage of each of these three pure compounds, called end-members.
The model has been used to study the performance of two CMC composites: a SiC (Nicalon) fibre-calcium aluminosilicate (CAS) matrix, 0°/90° cross-ply laminate Nicalon-CAS; and, carbon fibre-dual carbon-SiC matrix (C/C-SiC), plain weave laminate DLR-XT.
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