Rheniite

rheniite

cadmoindite

greenockite

wollastonite

Images

Formula: ReS2
Sulphide of rhenium, one of only two IMA-approved minerals that contain essential rhenium, the other one is tarkianite, (Cu,Fe)(Re,Mo)4S8. Rhenium is a transition metal that was originally thought to occur in the native state as tiny grains in wolframite from a Russian locality. It was later discredited because of uncertain origin (Mindat).
Crystal system: Triclinic
Specific gravity: 7.598 calculated
Streak: Grey-black
Colour: Silvery-white, black, red translucent
Environments

Fumeroles
Hydrothermal environments

Localities

At the Pagoni Rachi prospect, Alexandroupoli, Evros, Eastern Macedonia and Thrace, Greece, the Mo–Cu–Te–Ag–Au prospect is a porphyry-epithermal system hosted by a dacite porphyry and quartzfeldspar porphyry dikes. Rheniite and molybdenite, with very high contents of rhenium (up to 4.7 wt%), occur in quartz veins along with Fe–Cu sulphides, Pb-, Sn-, and Cl-bearing oxides, hematite, ilmenite and tellurides of bismuth. Earlier-formed gold-bearing quartz and magnetite veins with sodic–potassic–calcic alteration and late precious-metal telluride-rich carbonate–quartz veins with argillic alteration contain only minor amounts of molybdenite. The composition of rheniite ranges from almost pure rheniite with low Mo content to rheniite with up to 5.99 wt% Mo.
Rheniite and molybdenite likely precipitated as temperatures fell below 400°C during phase separation under relatively oxidising conditions, at elevated chlorine activity, and from relatively acid hydrothermal solutions. However, rheniite and Re-rich molybdenite may have formed directly from the vapour as sublimates, in a manner similar to the way they are deposited at the Kudriavy volcano, Kurile Islands (CM 47.5.1013-1036).

At the type locality, the Kudriavy volcano, Iturup Island, Kurilsky District, Kuril Islands, Sakhalin Oblast, Russia, rheniite occurs in the high temperature fumeraole as millimetric, wedge-shaped crystals that are dark red and translucent. Associated minerals include andradite, cadmoindite, corundum, garnet group minerals, greenockite, grossular, halite, magnetite, wollastonite and wurtzite (Mindat).
Rheniite from the Kudriavy Volcano - Image

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