Pf. Schofield et al., AN EXAFS STUDY OF CATION SITE DISTORTIONS THROUGH THE P2 C-P(1)OVER-BAR TRANSITION IN THE SYNTHETIC CUPROSCHEELITE SANMARTINITE SOLID-SOLUTION/, Mineralogical Magazine, 58(391), 1994, pp. 185-199
EXAFS-spectroscopy has been used to monitor changes in divalent cation
site geometries across P2/c-P1BAR phase transition in the sanmartinit
e (ZnWO4)-cuproscheelite (CuWO4) solid solution at ambient and liquid
nitrogen temperatures. In the ZnWO4 end member, Zn occupies axially-co
mpressed ZnO6 octahedra with two axial Zn-O bonds at approximately 1.9
5 angstrom and four square planar Zn-O bonds at approximately 2.11 ang
strom. The substitution of Zn by Cu generates a second Zn environment
with four short square planar Zn-O bonds and two longer axial Zn-O bon
ds. The proportion of the latter site increases progressively as the C
u content increases. Cu EXAFS reveals that the CuO6 octahedra maintain
their Jahn-Teller axially-elongate geometry throughout the majority o
f the solid solution and only occur as axially-compressed octahedra we
ll within the stability field of the Zn-rich phase with monoclinic lon
g-range order.