Xenotime

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Xenotime
Xenotímio1.jpeg
Xenotime from the Poços de Caldas alkaline massif, Brazil
General
Category Phosphate minerals
Formula
(repeating unit)
YPO4
Strunz classification 08.AD.35
Identification
Color Brown, brownish yellow, gray
Crystal habit Prismatic, radial aggregates, granular
Crystal system Tetragonal 4/m - dipyramidal
Cleavage Perfect [100]
Fracture Uneven to splintery
Mohs scale hardness 4.5
Luster Vitreous to resinous
Streak Pale brown, yellowish or reddish, to white
Diaphaneity Translucent to opaque
Specific gravity 4.4–5.1
Refractive index 1.720-1.815
Birefringence δ = 0.096
Pleochroism Dichroic
Other characteristics Not Radioactive or luminescent
References [1][2][3]

Xenotime is a rare earth phosphate mineral, whose major component is yttrium orthophosphate (YPO4). It forms a solid solution series with chernovite-(Y) (YAsO4) and therefore may contain trace impurities of arsenic, as well as silicon dioxide and calcium. The rare earths dysprosium, erbium, terbium, and ytterbium, and metal elements like thorium and uranium (all replacing yttrium) are the expressive secondary components of xenotime. Due to uranium and thorium impurities, some xenotime specimens may be weakly to strongly radioactive. Lithiophyllite, monazite, and purpurite are sometimes grouped with xenotime in the informal "anhydrous phosphates" group. Xenotime is used chiefly as a source of yttrium and heavy lanthanide metals (dysprosium, ytterbium, erbium, and gadolinium). Occasionally, gemstones are also cut from the finer xenotime crystals.

The etymology of the name xenotime is from the Greek words "κενός vain and τιμή honor because the yttrium contained within it was first thought to be a new element.[1][3] According to Vickery, the original name of the mineral was "kenotime", but due to a misprint, the "k" became an "x", and the change stuck.[citation needed] Xenotime was first described for an occurrence in Vest-Agder, Norway in 1832.[1]

Properties[edit]

Crystallising in the tetragonal (I41/amd) crystal system, xenotime is typically translucent to opaque (rarely transparent) in shades of brown to brownish yellow (most common), but also reddish to greenish brown and gray. Xenotime has a variable habit: It may be prismatic (stubby or slender and elongate) with dipyramidal terminations, in radial or granular aggregates, or rosettes. A soft mineral (Mohs hardness 4.5), xenotime is—in comparison to most other translucent minerals—fairly dense, with a specific gravity between 4.4–5.1. Its lustre, which may be vitreous to resinous, together with its crystal system, may lead to a confusion with zircon (ZrSiO4), that a similar crystal structure and with which xenotime may sometimes occur.

Xenotime has two directions of perfect prismatic cleavage and its fracture is uneven to irregular (sometimes splintery). It is considered brittle and its streak is white. The refractive index of xenotime is 1.720-1.815 with a birefringence of 0.095 (uniaxial positive). Xenotime is dichroic with pink, yellow, or yellowish brown seen in the extraordinary ray, and brownish yellow, grayish brown or greenish brown seen in the ordinary ray. There is no reaction under ultraviolet light. While xenotime may contain significant amounts of thorium or uranium, the mineral does not undergo metamictization like sphene or zircon would.

Occurrence[edit]

Occurring as a minor accessory mineral, xenotime is found in pegmatites and other igneous rocks, as well as gneisses rich in mica and quartz. Associated minerals include biotite and other micas, chlorite group minerals, quartz, zircon, certain feldspars, analcime, anatase, brookite, rutile, siderite, and apatite. Xenotime is also known to be diagenetic: It may form as minute grains or as extremely thin (less than 10 µ) coatings on detrital zircon grains in siliciclastic sedimentary rocks. The importance of these diagenetic xenotime deposits in the radiometric dating of sedimentary rocks is only beginning to be realised.[4]

Discovered in 1832, xenotime's type locality is Hidra (Hitterø), Flekkefjord, Vest-Agder, Norway. Other notable localities include: Arendal and Tvedestrand, Norway; Novo Horizonte, São Paulo, Novo Horizonte, Bahia, and Minas Gerais, Brazil; Madagascar; and California, Colorado, Georgia, and North Carolina, New Hampshire, United States. A new discovery of gemmy, colour change (brownish to yellow) xenotime has been reported from Afghanistan and been found in Pakistan. North of Mount Funabuse in Gifu Prefecture, Japan, a notable basaltic rock is quarried at a hill called Maru-Yama: Crystals of xenotime and zircon arranged in a radiating, flower-like pattern are visible in polished slices of the rock, which is known as chrysanthemum stone (translated from the Japanese kiku-ishi). This stone is widely appreciated in Japan for its ornamental value.

Small tonnages of xenotime sand are recovered, in association with Malaysian tin mining, etc., and are processed commercially. The lanthanide content is typical of "yttrium earth" minerals, and runs about two-thirds yttrium, with the remainder being mostly the heavy lanthanides, where the even-numbered lanthanides (such as Gd, Dy, Er, or Yb) each being present at about the 5% level, and the odd-numbered lanthanides (such as Tb, Ho, Tm, Lu) each being present at about the 1% level. Dysprosium is usually the most abundant of the even numbered heavies, and holmium is the most abundant of the odd numbered heavies. The lightest lanthanides are generally better represented in xenotime than the heaviest lanthanides are in monazite.

See also[edit]

References[edit]

  • Webster, R. (2000). Gems: Their sources, descriptions and identification (5th ed.), p. 182. Butterworth-Heinemann, Great Britain. ISBN