Wa. Dollase et Cr. Ross, CRYSTAL-STRUCTURES OF THE BODY-CENTERED TETRAGONAL TECTOSILICATES - K1.14MG0.57SI1.43O4, K1.10ZN0.55SI1.45O4, AND K1.11FE(1.11)3SI0.89O4, The American mineralogist, 78(5-6), 1993, pp. 627-632
The title compounds are isostructural stable phases that occur on bina
ry joins of mineralogic interest: SiO2-K2MgO2, SiO2-K2ZnO2, SiO2-KFeO2
; a corresponding phase occurs on the SiO2-KAlO2 join. The structure h
as I4mm symmetry, with cell dimensions a = 8.957 angstrom, c = 5.281 a
ngstrom (Mg phase). The eight Si plus Mg (or Zn, Fe) atoms per cell ar
e disordered over a single set of equivalent tetrahedrally coordinated
sites. The tetrahedra form four-membered rings further interconnected
into six- and eight-membered rings with two types of intervening larg
e cavity sites: K2 sites between facing four-membered rings are full,
but K1 sites in large, square channels show a smeared out partial occu
pancy probably caused by K-K repulsion. The body-centered tetragonal t
ectosilicate (BCTT) structure is structurally related to other major t
ectosilicates, though no natural occurrences are yet known.