gersdorffite


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gersdorffite

[′gerz‚dȯr‚fīt]
(mineralogy)
NiAsS A silver-white to steel-gray mineral, crystallizing in the isometric system; resembles cobaltite and may contain some iron and cobalt. Also known as nickel glance.
References in periodicals archive ?
Gersdorffite, a cobalt sulphide mineral, is apparently present as fine grains disseminated in pyrrhotite.
In the early 1980s, members of the Russell Society discovered a small pod of nickel minerals (nickeline, gersdorffite and millerite).
Sulfides generally crystallize during the last stage of mineralization in the cavities, along with graphite and zeolite minerals, and occur in two separate vein assemblages: (1) beryl-bearing fissure veins that carry accessory pyrite, pyrrhotite, sphalerite, chalcopyrite and trace amounts of galena, and (2) spodumene-bearing veins that host pyrite, pyrrhotite, molybdenite and trace amounts of gersdorffite.
Bou Azzer has produced the world's finest specimens of erythrite, roselite, roselite-beta, talmessite, wendwilsonite, skutterudite and gersdorffite.
Ernesto Ossolo had visited the classic mines of Bou Azzer and brought back fine nickeline and gersdorffite crystals.
Associated minerals are: scainiite, zinkenite, boulangerite, robinsonite, tintinaite, sorbyite and other incompletely characterized minerals, Other associated minerals are: sphalerite, cinnabar, galena, andorite, bournonite, tetrahedrite, chalcostibite, gersdorffite, barite, cerussite and stibiconite.
Associated minerals are: zinkenite, boulangerite, robinsonite, tintinaite, sorbyite, a new chloro-sulfosalt, sphalerite, cinnabar, galena, andorite, bournonite, tetrahedrite, chalcostibite, gersdorffite, barite, cerussite and stibiconite.
Gersdorffite is among the trace sulfides that have been identified as inclusions in bismuth nodules from the Bor pit.
has scored some gersdorffite from the Ait Hamane mine which surely is among the best yet for this rare nickel arsenide sulfide.
The mineralization consisted of patches, grains and intergrowths of argentite/acanthite, proustite, xanthoconite, smithite, miargyrite, argyrodite, unidentified bismuth sulfosalts (Gasparrini, 1978), jordanite, pyrargyrite and gersdorffite (Taylor, 1984).
Grains of impure gersdorffite to 15 microns have been noted in samples of sulfide-rich siliceous barite breccias collected from different locations in the southern part of the deposit.
Gersdorffite and nickeline occur with dolomite and as vein fillings which cut across the main upright cleavage and sulfide layering.