Raman spectra of the two high-pressure polymorphs of SiO2 (coesite and
stishovite) were investigated in the temperature range 105-875 K at a
tmospheric pressure. Coesite remained intact after the highest tempera
ture run, but stishovite became amorphous at temperatures above about
842 similar to 872 K. Most Raman modes exhibit a negative frequency sh
ift with temperature for these polymorphs, but positive trends were al
so observed for some modes. Except for some weak modes, nonlinear temp
erature variation were established for these poly morphs within the ex
perimental uncertainty and temperature range spanned. The slopes of th
e variation (delta V-i/delta T)(p) for these polymorphs were compared
with the published values. When compared with quartz and stishovite, t
he four-membered rings of SiO4-tetrahedra in coesite exhibit very litt
le change with both temperature and pressure. It is also suggested tha
t temperature and pressure should have opposite effects on the Raman s
hift of each vibrational mode.