Abstract
Tunisite, NaHCa2Al4[(CO3)4(OH)10] is a new carbonate found at the Pb – Zn deposit, Sakiet Sidi Youssef, Tunisia. It occurs in fine-grained white aggregates or in small tabular crystals associated with pyrite, marcasite, sphalerite and calcite in hydrothermal veins.
The new mineral is tetragonal; D74h – P4/nmm; a = 11.22 ± 0.01, c=6.582±0.001 Å, c/a=0.5866; V = 828.6 Å3, cell contents: 2{NaHCa2Al4[(CO3)4(OH)10.). The strongest lines in the X-ray powder photograph are: 5.615 (10), 2.592 (9), 3.551 (8), 3.288 (7), 2.526 (7) Å.
Tunisite is colorless. H = 4,5; ρ 2.51±0.02 (meas.), 2.48 (calc.). Basal and prismatic cleavage very good. Optically uniaxial (+), ω= 1.573 ± 0.001, ϵ= 1.599 ± 0.001.
The chemical analysis: Na2O 4.77, K2O 0.35, CaO 18.08, A12O3 32.56, CO2 28.66, H2O+ 15.04, H2O– 0.51, Σ 99.97 wt.%. DTA shows a strong endothermic peak at 440° (escape of 8CO2+7H2O) and an exothermic peak at 850° (formation of new crystalline phases and escape of 2H2O). IR spectrum shows absorption bands at 680 s, 850 s, 1155 s, 1530 vs, 1725 w, 1860 vw, 1920 w, 2330 vw, 2650 w, 3500 s cm−1.