Chemistry Reference
In-Depth Information
rather than corners with the immediately surrounding tetrahedra. However, the
predominant contacts involve corner-sharing, as in sphalerite.
We note that the split sites of these two structures are different: (As/Sn) for
colusite is in site 6
c
(Cu(2) in germanite) and (Fe/As) for germanite is in 8
e
(Cu(2)
in colusite). Figure
10c
shows the corresponding drawing for a sphalerite-like
component of Li
7
VN
4
involving only the V(1)N
4
, V(2)N
4
, Li(2)N
4
, Li(3)N
4
and
Li(5)N
4
tetrahedra, whereas it is the V(1)N
4
tetrahedra at the origins which share
edges. The close similarities are evident.
Here we are entering the whole complex realm of mineral chemistry where given
mineral structures can contain a variety of different substitutions. According to
colusite, whereas Sn, Sb, Fe and Ge are often present in significant quantities. Cu
content can vary somewhat.” The ideal, so-called high-tin colusite has the formula
Cu
26
[V
2
A
s
4
Sn
2
]S
32
, the As and Sn being disordered in the ratio of 2 to 1 on the 6
c
site of
P
43
n
, and this is the composition whose structure was reported. “Low-tin”
Fig. 10 (a) The structure of colusite (
a ¼
10.621
˚
) viewed along [111]. (As/Sn)S
4
tetrahedra -
green
,VS
4
tetrahedra -
grey
, Cu(2)S
4
tetrahedra -
light blue
, Cu(3)S
4
tetrahedra -
red
, Cu(1)S
4
tetrahedra -
purple
.(b) The equivalent structure of germanite (
a ¼
10.5862
˚
). Cu(2)S
4
tetra-
hedra -
green
, Cu(1)S
4
tetrahedra -
grey
, Cu(3)S
4
tetrahedra -
red
, (Fe/As)S
4
tetrahedra -
light
blue
, Cu(4)S
4
tetrahedra -
purple
.(c)Li
7
VN
4
[111] (
a
¼
9.606
˚
). V(1)N
4
tetrahedra -
grey
,
V(2)N
4
tetrahedra -
red
, Li(4)N
4
tetrahedra -
light blue
, Li(2)N
4
tetrahedra -
green
, Li(5)N
4
tetrahedra -
purple