Gelosaite

gelosaite

ferrimolybdite

koechlinite

sardignaite

Images

Formula: BiMo6+(2-5x)Mo5+6xO7(OH).H2O (0 < x < 0.4)
Hydrated molybdate, bismuth-bearing mineral
Crystal system: Monoclinic
Specific gravity: 5.114 calculated
Hardness: 3
Streak: White
Colour: Yellow, yellowish green, pale blue, colourless
Luminescence: Not fluorescent
Environments

Plutonic igneous environments
Hydrothermal environments

Gelosaite is a secondary mineral formed in the oxidation zone of bismuth-molybdenum deposits.

Localities

At Kingsgate, Gough Co., New South Wales, Australia, mineralisation is largely confined to quartz-rich pipes in leucogranite. Gelosaite was originally recovered from a single boulder of quartz from the waste dumps of the Old 25 pipe. Crystals up to 0.5 mm in size are tabular and range in colour from pale yellow and greenish yellow to pale blue. These occur perched on quartz crystals in vugs associated with bismutite. Nearly all gelosaite crystals from this locality are twinned (AM 96.268-273).
Gelosaite from Kingsgate - Image

At the type locality, Punta de Su Seinargiu, Sarroch, Metropolitan City of Cagliari, Sardinia, Italy, the deposits are related to leucogranitic intrusions. The only primary molybdenum-bearing mineral is molybdenite, associated with pyrite, bismuthinite, and sphalerite in quartz veins ranging from 5 to 15 cm thick and more rarely in the granite itself. Study of samples collected from small dumps yielded in addition native bismuth, cassiterite, anatase, brookite, aeschynite-(Ce), synchysite-(Ce), xenotime-(Y), bismoclite, ferrimolybdite, koechlinite, wulfenite, powellite and muscovite.
Only three small samples of gelosaite were found at the type locality, where it occurs in cavities in quartz veins within a granite rock. Gelosaite is a secondary mineral formed in the oxidation zone and is associated with sardignaite, ferrimolybdite, koechlinite, wulfenite and muscovite. It occurs as prismatic and very thin, elongated and tabular crystals up to 1 mm in length and a few micrometers across. Twinning was not observed in material from this locality (AM 96.268-273).
Gelosaite from Punta de Su Seinargiu - Image

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