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Millerite
(redirected from Nickel sulfide)

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millerite [′milĀ·ə‚rīt]
(mineralogy)
NiS A brass to bronze-yellow mineral that crystallizes in the hexagonal system and usually contains trace amounts of cobalt, copper, and iron; hardness is 3-3.5 on Mohs scale, and specific gravity is 5.5; it generally occurs in fine crystals, chiefly as nodules in clay ironstone. Also known as capillary pyrites; hair pyrites; nickel pyrites.

Millerite 

(named after the British crystallographer W. Miller [1801–80]), a mineral of the sulfide class; nickel sulfide, NiS, containing 64.7 percent Ni and 35.3 percent S. Millerite crystallizes in the trigonal system, forming characteristic slender brass-yellow hairlike crystals. It also forms fibrous, radiating, and other kinds of aggregates. Millerite has a hardness of 3–4 on Mohs’ scale and a density of 5,200–5,600 kg/m3. It occurs rarely in nature, usually in hydrothermal ore veins in association with other Ni and Co sulfides and arsenides, which are contained in copper-nickel ores (in Noril’sk and Monchegorsk in the USSR). Millerite is also formed during the sur-face weathering of nickel-bearing ultrabasic rocks by acidic surface waters saturated with H2S.

REFERENCE

Mineraly: Spravochnik, vol. 1. Moscow, 1960.


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He was one of the first scientists to suggest that iron sulfides and nickel sulfides might have held an important role in early life.
We have observed that the unique poly-metallic nature of the El Capitan deposit results in significant slag and/or cupellation losses when using lead collection fire assay, and the oxide nature of the deposit does not lend itself well to the application of nickel sulfide fire assays techniques typically used in sulfide PGM deposits.
Test work related to the impact of fine grinding on nickel sulfide collection of platinum group metal (PGM) values is ongoing and results will be reported upon receipt and verification.
 
 
 
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