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Nilanjan Bhowmick AIR 3, CSIR NET (Earth Science)
Rahul kumar
Andalusite, kyanite, and sillimanite are all naturally occurring aluminosilicate minerals that have the composition Al2SiO5 . The triple point of these three polymorphs is located at a temperature of 500 °C and a pressure of 0.4 GPa. These three minerals are commonly used as index minerals in metamorphic rocks. Each of these minerals occurs under different temperature-pressure regimes, and they are therefore rarely found together in the same rock. Because of this, the three minerals are a useful tool in identifying the pressure-temperature paths of the host rock in which they are found. At triple points, all of three phases of aluminosilicate can occur together in equilibrium.