Thallium leucite, TlAlSi 2 O 6 , has been synthesized at 4508C for 7 days, under ambient conditions, by the transformation of dehydrated analcime NaAlSi 2 O 6 in the presence of excess TlCl. This substitution of Tl for Na leads to confirmation of a thallium-leucite pseudomorph after analcime. Their optical properties, X-ray powder diffraction patterns, electron microprobe analysis, infrared spectra, and X-ray photoelectron spectroscopy have characterized the synthetic Tl-leucites. The IR spectra show that the mid-IR modes T-O stretching and T-O-T bending vibrations for TlAlSi 2 O 6 are more resemblant of those for analcime than for leucite, KAlSi 2 O 6 . This resemblance implies that Tl cation enters the W-site rather than the S-site in the analcime structure: Na (S)where & represents an S-site vacancy. The mechanism of this substitution is supported by the crystal chemical constraints: inasmuch as the S-site is smaller than the W-site, Tl + cations being larger than Na + plainly prefer the latter site to the former. One inference from the binding energy for Tl + by XPS is that Tl + occupies the extra-framework site in synthetic leucite pseudomorph, rather than the smaller tetrahedral site. The difference in Al/Si disordering between analcime and leucite and the nonstoichiometry due to the solid solution of the &Si 3 O 6 component into the leucite structure may provide a fundamental insight into understanding why TlAlSi 2 O 6 deviates from the trend defined by K-, Rb-and CsAlSi 2 O 6 leucite series on the a-c parameter diagram, inasmuch as these three cations in the leucite structure occupy the W-sites. Finally, synthesis of TlAlSi 2 O 6 leucite has an implication for the existence of other polymorphs due to different degrees of Al/Si disordering, except for high-and low-temperature leucites already known: natural leucites crystallized directly through igneous processes are different from those formed by substitution of K for Na in analcimes.