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Abstract
The crystal structure of pyrostilpnite from the Plaka mine, Lavrion Mining District, Greece, was refined in the space group
P
2
1
/
c
to a final
R
1
index of 0.0283 on the basis of 2047 reflections with
F
o
> 4σ(
F
o
) and 65 refined parameters. Unit-cell parameters of the crystal examined are
a
= 6.8629(6),
b
= 15.8800(14),
c
= 6.2711(5) Å, β = 117.087(2)°,
V
= 608.48(9) Å
3
and
Z
= 4. Chemical data agree with the stoichiometric formula Ag
3
SbS
3
. The crystal structure reported previously was confirmed, although a higher precision of refinement was achieved. It can be described as formed by {010} slabs running along
c
and connected along
a
through relatively longer Ag–S bonds. The analysis of the atomic displacement parameters together with a refinement with higher order tensors in the expression of the structure factors revealed no hint for pyrostilpnite as an ionic conductor. A historical background of the ‘ruby silvers’ is also reported.