Thorianite

thorianite

thorite

zircon

ilmenite

Images

Formula: ThO2
Oxide, uraninite group, forms a series with uraninite
Crystal System:
Specific gravity: 9.7 to 9.8
Hardness: 6½ to 7
Streak: Grey, grey-green to black
Colour: Black, brownish black, dark grey, dark reddish brown
Magnetism: Diamagnetic
Common impurities: U,Ce,La,Pb,TR
RADIOACTIVE
Environments

Pegmatites
Carbonatites
Metamorphic environments

Thorianite is an accessory mineral in granite pegmatites, and more rarely in carbonatites or serpentinite; it is commonly detrital in heavy mineral concentrates (HOM).

Localities

At the Andoloabo thorianite deposit, Belafa area, Maromby, Amboasary Sud, Anosy, Madagascar, thorianite is associated with phlogopite, diopside and spinel (HOM).

At the Turja peninsula, White Sea, Russia, thorianite occurs with pyrochlore as an accessory in the original calcite-diopside-hornblende and calcite-garnet-vesuvianite rocks.
As a rule, the calcite-diopside-hornblende rocks are medium to fine-grained aggregates of zeolites, calcite and apatite, including short prismatic and xenomorphic grains of diopside. Perovskite occurs as an accessory mineral. Evenly scattered in this polymineralic aggregate are rounded grains of magnetite and large (1-3 cm) poikilitic crystals of hornblende.
The calcite-garnet-vesuvianite rocks are composed of a fine-grained garnet-vesuvianite-phlogopite-calcite aggegate in which megacrysts( l-2 cm) of garnet and magnetite are uniformly distributed. Calcite also occurs in separate pockets. Perovskite is an accessory mineral (AM 59.378-380).

At the type locality, Balangoda, Ratnapura District, Sabaragamuwa Province, Sri Lanka, thorianite is an accessory mineral in granite pegmatites (Mindat). Associated minerals include thorite, zircon, ilmenite, cassiterite and allanite (HOM).

At Rose Road, Pitcairn, St. Lawrence county, New York, USA, thorianite mineralisation fluoresces brilliant green both from pieces of the original pod and from patchy coatings on the surfaces of other minerals that were down slope from the pod in fractured areas or as loose pieces in the scree (R&M 97.5.442).

Back to Minerals