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Figure 4
Experimental XANES spectra of (a) tridymite, (b) quartz and (c) stishovite for the Si K-edge region, and of (d) quartz-type GeO[_2] and (e) rutile-type GeO[_2] for the Ge K-edge region. The XANES spectra are useful for distinguishing between fourfold and sixfold coordination.

Journal logoJOURNAL OF
SYNCHROTRON
RADIATION
ISSN: 1600-5775
Volume 6| Part 5| September 1999| Pages 1051-1058
doi:10.1107/S0909049599005634
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