Phosphates, xenotime-(Y) forms a series with xenotime-(Yb) and with chernovite-(Y). Zircon is an epitaxial mineral (Mindat)
Physical data for xenotime-(Y), which is by far the more common mineral
Specific gravity: 4.4 to 5.1
Hardness: 4 to 5
Streak: Pale brown, yellowish or reddish, white
Colour: Yellowish brown, reddish brown, light red, flesh-red, light green, grey, greyish white, wine-yellow. Colourless to very light yellowish green, yellow or yellowish brown in transmitted light (Mindat)
Solubility: Very lightly attacked by acids
Xenotime is a rare phosphate of yttrium or
ytterbium that occurs as an accessory mineral in both acid and alkaline
rocks, and their associated pegmatites; it also occurs in mica,
and Alpine veins, and is a common detrital mineral in placers (HOM, Webmin, Dana). Associated minerals include
sillimanite, feldspar and
thorite (HOM, Dana, Mindat) and occasionally
fergusonite and columbite -
At Llallagua, Bolivia, xenotime has been found on monazite (MinRec 37.2.160).
At Trimouns quarry, France, xenotime is found, rarely, in small vugs in crystallised dolomite and calcite (MinRec 35.3.244).
At Erongo, Namibia, xenotime is associated with aquamarine, fluorite and quartz. It has also been found on metazeunerite from the uranium pocket (MinRec 37.5.454).
In the river alluvium in the Grey River-Mawheraiti River area, North Westland, New Zealand, xenotime has been found as a minor constituent of an assemblage that includes zircon, ilmenite, spessartite - almandine, monazite, and tantalum-rich cassiterite (AM 32.141).
At the type locality, Hidra, Flekkefjord, Norway, xenotime was found in a granite pegmatite associated with gadolinite, polycrase-euxenite, allanite, zircon, yttrotantalite and thorite (Dana).
At the Zagi mountain, Pakistan, xenotime, quartz and microcline have been found together on a specimen, with all three minerals having inclusions of astrophyllite (MinRec 35.3.219-220 ).
At Cheyenne Canyon, Pikes Peak, El Paso county, Colorado, USA, xenotime has been found with fluocerite and bastnäsite (Dana).
In the Manhattan schist, New York City, USA, xenotime and monazite crystals have been found in a vein of coarse-grained grey granite running through the local mica schist, and also in a pegmatite vein in the schist (R&M 84.3.236-237 )
At Polk, McDowell, Burke county, North Carolina, USA, xenotime occurs as a detrital mineral in placer gold deposits (Dana).
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