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Formula: UTi2O6
Valence: U4+Ti4+2O6
Oxide of uranium and titanium,
euxenite group
Crystal System: Orthorhombic
Specific gravity: 6.60 calculated
Hardness: 5 to 6
Colour: Brown-red, dark brown-red internal reflections
Common impurities: Th,Mn,Ca,Nd,TR
RADIOACTIVE
Environments
Localities
At the type locality, Fonte del Prete, San Piero in Campo, Campo nell'Elba, Livorno Province, Tuscany, Italy,
uranopolycrase occurs in a zoned pegmatite vein with
abundant Nb,Ta minerals and zeolites, near the contact with
granodiorite. The uranopolycrase is almost totally metamict.
Associated minerals include uranoan
polycrase-(Y), euxenite-(Y),
columbite-(Mn),
titanowodginite,
beryl,
stilbite, quartz,
orthoclase, albite,
lepidolite and elbaite
(HOM, Mindat).
Uranopolycrase from Fonte del Prete -
Image
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