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Published online by Cambridge University Press: 15 January 2025
Selenolaurite, ideally RuSe2, is a new mineral, the first natural ruthenium selenide. It was discovered in an assemblage with Se-bearing moncheite. Both form xenomorphic inclusions in the crystal aggregates of Os–Ir–Ru minerals found at the Ingul gold placer, Urals, Russia. In addition a mineral with selenolaurite composition was found as a euhedral inclusion within grains of Pt–Fe alloy with isoferroplatinum composition at the Kazan gold placer. These placers are situated in the Chelyabinsk district, South Urals, Russia. The selenolaurite from the Ingul placer forms interstitial grains with maximum size of section of 0.05–0.1 mm. Crystals of the selenolaurite from the Kazan placer reach 20 µm in size. Selenolaurite is grey with metallic lustre and is isotropic. Reflectance values [R (%) for COM approved wavelengths (nm)] are 45.8(470), 44.3(546), 43.8(589) and 43.1(650). The chemical composition of the holotype from the Ingul placer corresponds to the empirical formula (Ru0.99Ir0.05)Σ1.04(Se1.92Te0.03S0.01)Σ1.96. Selenolaurite is the selenium-dominant analogue of laurite, RuS2 with a pyrite-type structure. It is cubic, space group Pa3̅, a = 5.9424(2) Å, V = 209.84 2) Å3, Z = 4 and Dcalc. = 8.415 g·cm–3 (calculated on the basis of empirical formula and unit-cell parameters refined by the Rietveld method). The crystal structure has been refined from the powder data to RB = 0.0067. The strongest lines of the powder X-ray diffraction pattern [d(Å), (I), (hkl)] are: 3.434(41)(111), 2.973(90)(200), 2.6580(100)(210), 2.4264(84)(211) and 1.7913(87)(311). The possible sources of a Ru–Se mineralisation in the South Urals are ophiolitic ultramafic rocks enriched in Ru and depleted with sulfur.
Associate Editor: František Laufek
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