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Formula: Ni6Fe3+2(CO3)(OH)16.4H2O
Hydrated carbonate containing hydroxyl, hydrotalcite group,
hydrotalcite supergroup
Crystal System: Trigonal
Specific gravity: 2.80 to 2.88 measured, 2.83 calculated
Hardness: 2
Colour: Yellow to yellow-green
Environments
Localities
At the type locality, the Wolfe Creek meteorite crater, Carranya Station, Halls Creek Shire, Western Australia,
reevesite occurs as an
alteration product of the highly weathered iron-nickel meteorite,
forming yellow fine-grained aggregates lining cavities and cracks. Associated minerals include goethite,
nickel-bearing maghemite,
jarosite, nickel-bearing
serpentine, apatite and
lipscombite
(AM 52.1190-1197, HOM).
At the Bon Accord Nickel deposit, Barberton, Ehlanzeni District, Mpumalanga, South Africa, reevesite occurs as an alteration product of
violarite in nickel ore at a contact between
quartzite and ultramafic rocks. Associated
minerals include violarite, millerite, ferroan
trevorite, willemseite,
nimite, opal and
quartz
(AM 56.1077-1081, HOM, Dana).
At Hagdale Quarry, Unst, Shetland, Scotland, UK, reevesite occurs on chromatite
associated with honessite, hydrohonessite and
theophrastite
(HOM).
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