CRYSTAL-STRUCTURES OF THE BODY-CENTERED TETRAGONAL TECTOSILICATES - K1.14MG0.57SI1.43O4, K1.10ZN0.55SI1.45O4, AND K1.11FE(1.11)3SI0.89O4

Citation
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
Citations number
18
Categorie Soggetti
Geology,Mineralogy
Journal title
ISSN journal
0003004X
Volume
78
Issue
5-6
Year of publication
1993
Pages
627 - 632
Database
ISI
SICI code
0003-004X(1993)78:5-6<627:COTBTT>2.0.ZU;2-H
Abstract
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.