XENOTIME

    Class : Phosphates, arsenates, vanadates
    Subclass : Anhydrous phosphates
    Crystal system : Tetragonal
    Chemistry : YPO4
    Rarity : Uncommon


Xenotime is a relatively rare mineral. It is found mainly as an accessory mineral in granites, and in larger crystals in pegmatites where it is difficult to distinguish from zircon. More rarely, it is observed in alkaline granites and alpine clefts : its deposits are comparable to those of monazite. Its chemical composition is fluctuating, with yttrium being able to be replaced in significant quantities by rare earths (lanthanum, neodymium), thorium, uranium or zirconium. Despite the presence of radioactive elements, xenotime is never metamict. unalterable, it can concentrate in large placers that are sometimes exploitable. Its name comes from the Greek xenos (foreigner) and time (honor) because of the rarity of the mineral. Xenotime occurs in tetragonal prisms ending in two pyramids like zircon. It also has the same brown, yellow-brown or reddish color as the latter. It is an ore of yttrium, often recovered as a by-product in alluvial mining.

Main photo : Xenotime from Novo Horizonte, Bahia, Brazil © Tony Peterson

Xenotime from Zagi Mountain, Pakistan © Dan Weinrich
Xenotime from Hiltveit, Norway © The Collection of Iveland Municipality
Xenotime from Mount Malosa, Malawi © Bruno Marello
Xenotime from Trimouns, Ariège, France © François Garric

Xenotime in the World

The largest known xenotime crystals measure 5 cm and come from a pegmatite near Ibitiara (Bahia, Brazil) and Zagi Mountain (Pakistan). The Blomerus pegmatite (South Africa) contains magnificent crystals that reach 2 cm. Large crystals also come from the Yazgulem mountains in Tajikistan and the alluvium of the Betsiboka River (Madagascar). The pegmatites of the Arendal region, in southern Norway, contain significant quantities of xenotime, which are the origin of important alluvial placers.

Xenotime in France

In France, xenotime is known in millimeter-sized crystals in the hydrothermalized dolomites of Trimouns (Ariège) and in the alpine clefts of Plan du Lac (Isère). It is also found in numerous alluviums.

Twinning

Twinning is known on {111} but is rare.

Fakes and treatments

No fakes listed for this mineral species.



Hardness : 4 to 5
Density : 4.4 to 5.1
Fracture : Irregular
Streak : White, brown, yellow or red


TP : Translucent to opaque
RI : 1.720 to 1.827
Birefringence : 0.096
Optical character : Uniaxial +
Pleochroism : Low
Fluorescence : None


Solubility : Insoluble

Magnetism : ParamagneticRadioactivity : Very low

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