Full multiple-scattering (MS) calculations of the X-ray absorption spe
ctra at the silicon L(2,3), K and oxygen K-edges in zircon and alpha-q
uartz and comparison to ELNES and XANES experimental data are used to
elucidate the fine structure in the spectra. The pronounced difference
s between the quartz vs zircon spectra are mostly in the intensities o
f the transitions, not in their energies but can be fully modelled wit
h the MS approach. It is shown that the intensities are related to the
different site symmetries in these structures. Copyright (C) 1996 Els
evier Science Ltd