EXAFS spectroscopy has been used to monitor changes in divalent cation site geometries across the P2/c-Pi phase transition in the sanmartinite (ZnWO4)-cuproscheelite (CuWO4) solid solution at ambient and liquid nitrogen temperatures. In the ZnWO4 end member~ Zn occupies axially-compressed ZnO6 octahedra with two axial Zn--O bonds at approximately 1.95 A and four square planar Zn-O bonds at approximately 2.11 A. 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 bonds. The proportion of the latter site increases progressively as the Cu content increases. Cu EXAFS reveals that the CuO6 octahedra maintain their Jahn-Teller axially-elongate geometry throughout the majority of the solid solution and only occur as axially-compressed octahedra well within the stability field of the Zn-rich phase with monoclinic long-range order.KEVWORDS: EXAFS spectroscopy, sanmartinite, cuproscheelite, phase transition.
In~oducfionREciter powder X-ray diffraction studies on the complete solid solution between sanmartinite, ZnWO4, and cuproscheelite, CuWO4, have revealed the existence of a displacive ferroelastic phase transition Redfern, 1992, 1993). The spontaneous strain, calculated from the lattice parameters, was used as a measure of the order parameter for the transition which, at room *Present Address: Department of Mineralogy, Natural History Museum, Cromwell Road, London SW7 5BD, UK temperature, appeared continuous as a function of composition and with a critical composition of Cu0.22Zn0.78WO4 . With increasing Cu-content and temperature, the transition was found to become more first-order in character with a tricritical transition occurring at about Zn0.32Cuo.68WO 4 and 650~The observed critical transition temperature varied non-linearly as a function of composition indicating a coupling between X, the molar fraction CuWO4, and the order parameter, Q, of the form ~IXQ 2 + ~2XQ 4. The resulting Landau potential successfully modelled the transition as a function of both composition and temperature.