| Библ. ссылка: | Barkov A.Y., Tolstykh N.D., Martin R.E., McDonald A.M. Tamuraite, Ir5Fe10S16, a New Species of Platinum-Group Mineral from the Sisim Placer Zone, Eastern Sayans, Russia // MINERALS. - 2021. - Vol.11. - Iss. 5. - Art.545. |
| Реферат: | eng: Tamuraite, ideally Ir5Fe10S16, occurs as discrete phases (<= 20 mu m) in composite inclusions hosted by grains of osmium (<= 0.5 mm across) rich in Ir, in association with other platinum-group minerals in the River Ko deposit of the Sisim Placer Zone, southern Krasnoyarskiy Kray, Russia. In droplet-like inclusions, tamuraite is typically intergrown with Rh-rich pentlandite and Ir-bearing members of the laurite-erlichmanite series (up to similar to 20 mol.% "IrS2"). Tamuraite is gray to brownish gray in reflected light. It is opaque, with a metallic luster. Its bireflectance is very weak to absent. It is nonpleochroic to slightly pleochroic (grayish to light brown tints). It appears to be very weakly anisotropic. The calculated density is 6.30 g center dot cm(-3). The results of six WDS analyses are Ir 29.30 (27.75-30.68), Rh 9.57 (8.46-10.71), Pt 1.85 (1.43-2.10), Ru 0.05 (0.02-0.07), Os 0.06 (0.03-0.13), Fe 13.09 (12.38-13.74), Ni 12.18 (11.78-13.12), Cu 6.30 (6.06-6.56), Co 0.06 (0.04-0.07), S 27.23 (26.14-27.89), for a total of 99.69 wt %. This composition corresponds to (Ir2.87Rh1.75Pt0.18Ru0.01Os0.01)(sigma 4.82)(Fe4.41Ni3.90Cu1.87Co0.02)(sigma 10.20)S-15.98, calculated based on a total of 31 atoms per formula unit. The general formula is (Ir,Rh)(5)(Fe,Ni,Cu)(10)S-16. Results of synchrotron micro-Laue diffraction studies indicate that tamuraite is trigonal. Its probable space group is R3m (#166), and the unit-cell parameters are a = 7.073(1) angstrom, c = 34.277(8) angstrom, V = 1485(1) angstrom(3), and Z = 3. The c:a ratio is 4.8462. The strongest eight peaks in the X-ray diffraction pattern [d in angstrom(hkl)(I)] are: 3.0106(216)(100), 1.7699(420)(71), 1.7583(2016)(65), 2.7994(205)(56), 2.9963(1010)(50), 5.7740(102)(45), 3.0534(201)(43) and 2.4948(208)(38). The crystal structure is derivative of pentlandite and related to that of oberthurite and torryweiserite. Tamuraite crystallized from a residual melt enriched in S, Fe, Ni, Cu, and Rh; these elements were incompatible in the Os-Ir alloy that nucleated in lode zones of chromitites in the Lysanskiy layered complex, Eastern Sayans, Russia. The name honors Nobumichi Tamura, senior scientist at the Advanced Light Source of the Lawrence Berkeley National Laboratory, Berkeley, California.
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