F. Farges, FIVEFOLD-COORDINATED TI4- A NEW OCCURRENCE SHOWN BY TI K-EDGE XANES SPECTROSCOPY( IN METAMICT ZIRCONOLITE AND TITANITE ), The American mineralogist, 82(1-2), 1997, pp. 44-50
The coordination environments of Ti in two fully metamict zirconolite
samples and two partially metamict titanite samples were determined us
ing high-resolution, X-ray absorption near-edge structure (XANES) spec
troscopy at the Ti K edge. Fivefold-coordinated Ti is the dominant Ti
species in the zirconolite samples (similar to 80 +/- 10% of the total
Ti atoms). This unusual Ti coordination is also possible in the titan
ite samples. No significant evidence for Ti-[4] was found in any of th
e samples studied. Comparison with other amorphous materials, such as
other metamict minerals (aeschynite and pyrochlore) and titanosilicate
glasses and melts, suggests that fivefold coordination is rather comm
on for Ti4+ in aperiodic structures. However, the metamict state is ch
aracterized by the presence of unusual trigonal bipyramids around Ti-[
5](4+).