Forsterite has an unusually high melting temperature at atmospheric pressure, almost, but the melting temperature of fayalite is much lower ( about ).
12.
Fayalite is stable with quartz at low pressures, whereas more magnesian olivine is not, because of the reaction olivine + quartz = orthopyroxene.
13.
Therefore, the gas atmosphere in furnace can be calculated through the ratio of magnetite / fayalite in slag ( Hauptmann 2007, 22 ).
14.
Green sand for aluminum typically uses olivine sand ( a mixture of the minerals forsterite and fayalite, which is made by crushing dunite rock ).
15.
In this reducing environment, the silicon in the clay reacts with wustite to form fayalite and, at around, the fayalite will become a liquid.
16.
In this reducing environment, the silicon in the clay reacts with wustite to form fayalite and, at around, the fayalite will become a liquid.
17.
Through the shape of fayalite, cooling rates of the slag can be roughly estimated ( Donaldson 1976, cited in Etller et al . 2009 ).
18.
In the olivine structure, the main olivine series of ( Mg, Fe ) 2 SiO 4 consist of magnesium-rich forsterite and iron-rich fayalite.
19.
The temperature at which the liquidous phases crystallize in a sequence : mullite + tridymite, followed by sekaninaite and finally fayalite + clinoferrosilite ( Grapes, 2010 ).
20.
Because iron ( II ) ions were oxidized in the Stromboli magma, little iron ( II ) was available to form Fe-rich olivine ( fayalite ).
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