Talc is a clay mineral belonging to the phyllosilicate family. It has the empirical formula of Mg3Si4O10(OH)2 and the chemical name of Magnesium silicate hydroxide.
Taken from http://mineral.galleries.com
Talc is composed of layers of silicate - (SiO4)-4 and brucite - Mg2(OH)2.
It has a uniform composition with little or no atomic substitution. Derived from ultrabasic igneous rocks or found in some soil fractions, it is classified as a low to medium metamorphic rock.
Talc decomposes at 750 degrees centigrade and 1kbar pressure in two steps;
7Mg3Si4O10(OH)23Mg7Si8O22(OH)2
+ 4SiO2 +4H2O (1)
Talc
anthophyllite(an amphibole) + quartz + vapour
Mg7Si8O22(OH)27MgSiO3
+ SiO2 +H2O (2)
Anthophyllite
enstatite + quartz + vapour
Enstatite is more stable above 750 degrees but under equilibrium conditions (eg at 750 degrees) it takes an average of 6 months to become 50% complete.