Vinciennite Cu10Fe4Sn(As0.8Sb0.2)S16 was discovered in the pyrite deposit in Chizeuil, Saône-et-Loire, France. It is associated with pyrite, chalcopyrite, colusite, stannite, bornite, enargite, tetrahedrite, tennantite and other minerals in a gangue of quartz and/or barite. Other minerals include : hessite, altaite, tetradymite, cassiterite, stannoidite, kesterite, mawsonite, aikinite, cosalite, bismuthinite, wittichenite, bismuth, molybdenite, rutile, chalcocite and covellite. Vinciennite also has been found at Huaron, Peru. As small opaque grains up to 1 mm, with a metallic lustre and an orange colour ; VHN25 = 280, calculated density 4.29 g.cm-3. Very brittle with a conchoidal fracture. In polarized light, the anisotropism is weak with colours ranging from purplish-blue to greenish brown-yellow ; simple or weakly polysynthetic twins are occasionally observed. The reflectance values are (SiC standard) : 420 nm : 19.4-19.4 ; 460 nm : 21.8-20.6 ; 500 nm : 23.9-22.8 ; 540 nm : 27.7-26.5 ; 580 nm : 30.7-29.5 ; 620 nm : 33.6-32.1 ; 660 nm : 35.9-34.3 ; 700 nm : 37.8-36.0 ; 740 nm : 38.8-36.8 ; 780 nm : 39.5-36.6. Pseudo-cubic, vinciennite is in fact tetragonal P4122 (or possibly P4/mmm, P422 or P4mm) with a = b = c = 10.697(6) Å and Z = 2. Strongest lines of the X-ray powder diagram are : 4.37 (3) 211 ; 3.088 (10) 222 ; 2.676 (5) 400-004 ; 1.895 (9) 440-404 ; 1.614 (7) 622-226 ; 1.227 (4) 626-662 ; 1.091 (5) 844-448. Analytical results (mean of 6 analyses) with a cameca electron microprobe using Sb2S3, SnO2, As, Cu and Fe as standards are : Cu 40.90 ; Fe 14.63 ; Sn 7.33 ; As 3.43 ; Sb 1.60 ; S 31.85 ; total 99.74 %. The name is for Prof. Henri Vincienne (1898-1965) who first called attention to the mineral. Type material is preserved in the mineralogical collection of the Ecole Nationale Supérieure des Mines de Paris. Its description was approved by I. M. A.
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