Optical second-harmonic-generation (SHG) and Raman scattering experime
nts have been performed on quartz up to pressures of 31 GPa. The SHG s
ignal and its anisotropy were found to remain approximately constant u
p to about 22 GPa at which value the SHG showed a discontinuous decrea
se in magnitude, consistent with a phase transition at that pressure.
An increase in pressure beyond 22 GPa produced a linear decrease in th
e SHG signal and its anisotropy. The observation of SHG above 22 GPa i
ndicates that at least one of the crystalline phases of SiO2 stable at
those pressures lacks inversion symmetry. A significant SHG signal wa
s detected at 31 GPa, indicating that quartz is not entirely amorphous
at that pressure with respect to a macroscopic nonlinear dipole momen
t.