File:Kyanite-Sillimanita-Andalusite diagram.svg

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Description The stability fields of the Al2SiO5 minerals polymorphs. 1, 2 and 3 are the stability fields of Kyanite, Andalusite and Sillimanite respectively. TP is the triple point, where, theoretically the three aluminosilicates minerals exist in equilibrium. The Y axis is the pressure in kbar and the X axis is the temperature in Celsius grades.
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Author Eurico Zimbres
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current18:46, 24 May 2007Thumbnail for version as of 18:46, 24 May 2007778 × 645 (21 KB)Zimbres (talk | contribs){{Information |Description= The stability fields of the Al<sub>2</sub>SiO<sub>5</sub> minerals polymorphs. 1, 2 and 3 are the stability fields of Kyanite, Andalusite and Sillimanite respectively. TP is the triple point, where, theoretically the three alum

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