T. Baliczunic et al., CONTRIBUTIONS TO THE CRYSTAL-CHEMISTRY OF THALLIUM SULFOSALTS .3. THECRYSTAL-STRUCTURE OF LORANDITE (TLASS2) AND ITS RELATION TO WEISSBERGITE (TLSBS2), Neues Jahrbuch fur Mineralogie. Abhandlungen, 168(3), 1995, pp. 213-235
Crystal structure of lorandite TLAsS(2) was refined from single crysta
l data using 793 independent reflections (final R = 0.071). ZEAMANN &
ZEMANN'S (1959) and FLEET's (1973) model was confirmed and further ref
ined; current refinement yields average Tl-S and As-S distances equal
to 3.30 Angstrom and 2.28 Angstrom, respectively. Structure of lorandi
te is related to the SnS archetype but it differs from all the other S
nS-related sulphosalt structures by its distinct layer stacking. Confi
gurations of the (100) layer surfaces of lorandite are very similar to
those on (010) layer surfaces of weissbergite (TlSbS2). These surface
s contain Tl-S double strands that alternate with strips that comprise
As-S (resp. Sb-S) chain fragments; their mesh is rectangular for lora
ndite but oblique for weissbergite. Microprobe and powder diffraction
data on the system TlAsS2-TlSbS2 show miscibility gaps between 54 and
85 mol% TlAsS2 and (probably) also between 24 and 34 mol% TLAsS(2) for
syntheses at 250 degrees C. Lorandite and As-poor weissbergite are se
parated by a triclinic ''weissbergite-like phase'' TlAs0.34-0.54Sb0.66
-0.46S2 with a (probably) ordered As and Sb distribution.