The thermal reactivity of the naturally occurring silicates jadeite, N
aAl[Si2O6], and nephrite, a variety of actinolite, Ca2(Mg,Fe)5[(OH,F)S
i4O11]2, have been investigated by thermogravimetric and thermomechani
cal analysis as well as temperature-dependent X-ray diffraction and an
alytical electron microscopy. TG shows that nephrite undergoes a weigh
t loss at around 900-degrees-C. Mass spectrometry reveals that this ir
reversible reaction corresponds to the evolution of H2O, and XRD shows
that a phase related to diopside CaMg[Si2O6] is formed. Jadeite does
not undergo any observable weight changes up to 1000-degrees-C. Thermo
mechanical analysis indicates a reversible phase transition at about 9
50-degrees-C. Temperature-dependent X-ray diffraction shows that jadei
te is again present on cooling (peak temperature: 1000-degrees-C), but
that this is accompared by an additional unidentified phase. The mech
anism of this process is not yet clear although it has been observed i
n several samples from different origins and with different metal impu
rities.