Karelianite

karelianite

pyrrhotite

tremolite

titanite

Images

Formula: V2O3
Simple oxide of vanadium, hematite group
Crystal System: Trigonal
Specific gravity: 4.95 calculated
Hardness: 8 to 9
Streak: Black
Colour: Black
Common impurities: Fe,Cr
Environments

Metamorphic environments
Hydrothermal environments

Localities

At Shanglin County, Nanning, Guangxi, China, karelianite occurs in vanadiferous pyrobitumen (anthraxolite), associated with millerite, violarite and montroseite (HOM).

At the type locality, the Outokumpu mining district, North Karelia, Finland, karelianite occurs in sulphide-rich portions of glacial boulders derived from high-grade metamorphic rocks, as schists and quartzites. Associated minerals include pyrrhotite, chalcopyrite, pyrite, tremolite, graphite, titanite and quartz (HOM).


At the Mounana Mine, Mounana, Léboumbi-Leyou Department, Haut-Ogooué Province, Gabon, karelianite occurs in primary unoxidised uranium-vanadium ores. Associated minerals include corvusite, montroseite, uraninite and quartz (HOM).

At Buca della Vena Mine, Pontestazzemese, Stazzema, Lucca Province, Tuscany, Italy, karelianite is found associated with dessauite in alpine hydrothermal veins developed in a hematitebaryte ore within dolostone (CM 46.5.1183-1194).

At Ol'khonskiye Vorota Strait, Irkutsk Oblast, Russia, there is a continuous solid solution series between the two end-members eskolaite and karelianite. Members of that series in association with schreyerite, olkhonskite and rutile are reported in the graphite-bearing sillimanite quartzite schists (CM 46.5.1183-1194).

At the Merelani Hills, Lelatema Mountains, Simanjiro District, Manyara Region, Tanzania, grains of karelianite are found at the contact with pyrrhotite as a discontinuous rim up to 700 mm wide, or as an infilling phase in corroded zones of the pyrrhotite. The crystals are free of inclusions but are in some cases partly intergrown with vanadian phlogopite. Compositions are very close to the karelianite end-member of the solid solution (CM 46.5.1183-1194).

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