Fe. Wagner et al., AU-197 MOSSBAUER STUDY OF THE GOLD-SILVER DITELLURIDES SYLVANITE, KRENNERITE AND CALAVERITE, Canadian Mineralogist, 32, 1994, pp. 189-201
Mossbauer spectroscopy of the 77.3 keV gamma-rays of Au-197 was used t
o investigate the gold ditellurides sylvanite AuAgTe4, krennerite Au1-
xAgTe2 (x almost-equal-to 0.2) and calaverite AuTe2. The gold ditellur
ides have been found to exhibit distinctive Mossbauer spectra that can
be explained by different amounts of gold on the (4+2) and (2+2+2) ty
pe of sites, with the former occupied only by gold, and the latter by
gold as well as silver. The Lamb-Mossbauer factors of the (2+2+2) site
s were found to be 75% or less of those for the (4+2) sites. The overa
ll Lamb-Mossbauer factors for sylvanite, krennerite and calaverite are
only about 60% of the Lamb-Mossbauer factor for metallic gold.