Abstract
Ferrotorryweiserite, Rh5Fe10S16, occurs as small grains (≤20 µm) among droplet-like inclusions (up to 50 μm in diameter) of platinum-group minerals (PGM), in association with oberthürite or Rh-bearing pentlandite, laurite, and a Pt-Pd-Fe alloy (likely isoferroplatinum and Fe-Pd-enriched platinum), hosted by placer grains of Os-Ir alloy (≤0.5 mm) in the River Ko deposit. The latter is a part of the Sisim placer zone, which is likely derived from ultramafic units of the Lysanskiy layered complex, southern Krasnoyarskiy kray, Russia. The mineral is opaque, gray to brownish gray in reflected light, very weakly bireflectant, not pleochroic to weakly pleochroic (grayish to light brown tints), and weakly anisotropic. The calculated density is 5.93 g·cm–3. Mean results (and ranges) of four WDS analyses are: Ir 18.68 (15.55–21.96), Rh 18.34 (16.32–20.32), Pt 0.64 (0.19–1.14), Ru 0.03 (0.00–0.13), Os 0.07 (0.02–0.17), Fe 14.14 (13.63–14.64), Ni 13.63 (12.58–14.66), Cu 4.97 (3.42–6.41), Co 0.09 (0.07–0.11), S 29.06 (28.48–29.44), and total 99.66 wt.%. They correspond to the following formula calculated for a total of 31 atoms per formula unit: (Rh3.16Ir1.72Pt0.06Ru0.01Os0.01)Σ4.95(Fe4.48Ni4.11Cu1.38Co0.03)Σ10.00S16.05. The results of synchrotron micro-Laue diffraction studies indicate that ferrotorryweiserite is trigonal; its probable space group is R3¯m (#166) based on its Ni-analog, torryweiserite. The unit-cell parameters refined from 177 reflections are a = 7.069 (2) Å, c = 34.286 (11) Å, V = 1484 (1) Å3, and Z = 3. The c:a ratio is 4.8502. The strongest eight peaks in the X-ray diffraction pattern derived from results of micro-Laue diffraction study [d in Å(hkil)(I)] are 2.7950 (202¯5) (100); 5.7143 (0006) (60); 1.7671 (224¯0) (44.4); 3.0486 (202¯1) (39.4); 5.7650 (101¯2) (38.6); 2.5956 (202¯7) (37.8); 3.0058 (112¯6) (36.5); and 1.5029 (42¯ 2¯12) (35.3). Ferrotorryweiserite and the associated PGM crystallized from microvolumes of residual melt at late stages of crystallization of grains of Os- and Ir-dominant alloys occurred in lode zones of chromitites of the Lysanskiy layered complex. In a particular case, the residual melt is disposed peripherally around a core containing a disequilibrium association of magnesian olivine (Fo72.9–75.6) and albite (Ab81.6–86.4), with the development of skeletal crystals of titaniferous augite: Wo40.8–43.2En26.5–29.3Fs20.3–22.6Aeg6.9–9.5 (2.82–3.12 wt.% TiO2). Ferrotorryweiserite represents the Fe-dominant analog of torryweiserite. We also report occurrences of ferrotorryweiserite in the Marathon deposit, Coldwell Complex, Ontario, Canada, and infer the existence of the torryweiserite–ferrotorryweiserite solid solution in other deposits and complexes.
Highlights
Ferrotorryweiserite, Rh5 Fe10 S16, is a new mineral species discovered in the RiverKo suite, which represents part of the Sisim placer zone, south of Krasnoyarsk, Krasnoyarskiy kray, Russia
Ferrotorryweiserite occurs as small grains (≤20 μm), which are portions of composite, droplet-like inclusions of platinum-group minerals (PGM), mainly oberthürite or pentlandite enriched in Rh, laurite, Pt-(Pd)-Fe alloy, braggite-vysotskite, vasilite, and chalcopyrite, hosted by placer grains of Os- or
Our results indicate that the mineral is trigonal, and the probable space group, R3m
Summary
Ferrotorryweiserite, Rh5 Fe10 S16 , is a new mineral species discovered in the RiverKo suite, which represents part of the Sisim placer zone, south of Krasnoyarsk, Krasnoyarskiy kray, Russia (approximate location 54◦ 450 N, 93◦ 090 E). Ferrotorryweiserite is related to tamuraite, Ir5 Fe10 S16 , and kuvaevite, Ir5 Ni10 S16 [5,6], which are other members of the torryweiserite family that occur as inclusions in grains of Os-Ir alloy in heavy-mineral fractions of platinum-group minerals (PGM) in the placer zone of the Sisim river and its tributaries, rivers Ko and. In relation to the series of ferrotorryweiserite–torryweiserite, we document an unusual occurrence of the association olivine-albite (Fo73–76 and Ab82–86 ) developed in the core of a globular inclusion hosted by a grain of iridium from the River Ko. Additional occurrences of members of the ferrotorryweiserite-torryweiserite series are expected in a variety of ore deposits associated with ultramafic-mafic complexes that are known to contain Rh- and Ir-based species of PGM, cf [10,11] Additional occurrences of members of the ferrotorryweiserite-torryweiserite series are expected in a variety of ore deposits associated with ultramafic-mafic complexes that are known to contain Rh- and Ir-based species of PGM, cf. [10,11]
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