ABSTRACT
The Raman spectra, x-ray photoelectron spectroscopy (XPS), and x-ray excited luminescence spectra of crystalline quartz samples subjected to different pressure levels through detonation were compared with the spectra of the original samples. In the samples under study, the luminescence of a self-trapped exciton (STE) was analyzed, which, when excited by x-rays, has a high energy yield (â¼20%) in crystallineα-quartz not treated by detonation. The deviations of the luminescence spectrum are small in the pressure range from 9 to 27 GPa relative to untreated samples, which means the presence of crystalline quartz grains. A sharp change in the spectrum occurs for the sample subjected to a pressure of 34 GPa. The STE band practically disappeared and a band appeared at 350 nm. This band appears in thermally stimulated luminescence (in contrast to the STE band, which is not observed at all in thermally stimulated luminescence) and, therefore, can be attributed to some defects arising due to high pressure. This luminescence is not similar to the luminescence of a stishovite single crystal, but analysis of the XPS spectra suggests the formation of non-crystalline stishovite in detonated samples. In the Raman scattering spectra, a single sharp line at 465 cm-1, characteristic ofα-quartz, was observed in the samples after detonation pressure for the remaining small crystal grains. This line decreased greatly for the sample subjected to a pressure of 34 GPa. Against the structureless background of exposed samples of 'poor' optical quality, other Raman bands did not appear. It can be assumed that there are very broad bands of Raman scattering caused by the amorphization of stishovite under high detonation pressure. Amorphization explains the absence of luminescence, similar to the stishovite crystal.
