“…Its structure has been investigated by Ghose and Wan (1978) and Marr and Glasser (1979), whose studies revealed that zektzerite contains a six-repeat unit double chain silicate anion ('sechserdoppelkette') and that a wide variety of cation substitutions is possible. Thus zektzerite, LiNaZrSi6015 is isostructrual with tuhualite, (Na,K)2Fe4Si12030 (Merlino, 1969), emeleusite, Na2LiFeSi6015 (Upton et al, 1978), LizZrSi6Ox5 (Quintana and West, 1981), and a series of phases of the general formula LiNa2M3+Si6015, where M 3+ = Fe,Cr, Sc,In,Y,(Yb + Lu),Er,Ho,Dy,Gd,Sm (Marr and Glasser, 1979). Therefore, there is considerable scope for the incorporation of a number of cations of radiological significance in the zektzerite structure, although the mineral synthesized in these experiments only included trace amounts of Zn, Mo, and U Savage and Chapman, 1982).…”