“…The structures of the lillianite-type chalcogenides can be denoted as L(n,n 0 ), in which n and n 0 are the numbers of metal sites in the octahedral chains of the two alternating slabs; the different members of the lillianite series vary in the thickness of the NaCl-type blocks. Many naturally occurring minerals and synthetic lillianite-type or special case of Pavonite series [P(N,1)] chalcogenides have been studied, including PbBi 4 S 7 [L(2,1)] [16]; CuBi 5 S 8 [L(3,1)] [17]; Cu 3.21 Bi 4.79 S 9 [L(4,1)] [18]; AgBi 3 S 5 [L(5,1)] [19]; Pb 3 Bi 2 S 6 [9,20], AgPbBi 3 S 6 [21], and AgPbSb 3 S 6 [L(4,4)] [22]; Ag 5 Pb 8 Bi 13 S 30 [L(4,7)] [23]; Pb 6 Bi 2 S 9 [24] and K 0.54 Sn 4.92 Bi 2.54 Se 9 [L(7,7)] [25]; Ag 3 Bi 7 S 12 [L(7,1)] [26]; KSn 5 Bi 5 Se 13 [L(4,5)] [25]; Ag 7 Pb 6 Bi 15 S 32 [L (4,8)] [27]; Ag 7 Pb 10 Bi 15 S 36 [L (5,9)] [10]; and Ag 12.5 Pb 15 Bi 20.5 S 52 [L (11,11)] [11]. Most of the above lillianite and Pavonite type chalcogenides are sulfosalts; only a few selenides have been reported.…”