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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.
The xenotime group is a grouping of minerals containing anhydrous phosphates and vanadates. Xenotime group members. Members of the xenotime group include: [1]
The mineral species Xenotime-(Gd) was approved by the IMA in 2023, [3] a description of the mineral was published in 2024 based on crystals found within gadolinium rich xenotime-(Y) sampled at the Zimná Voda quartz vein near Prakovce. [4] Besides yttrium, the examined type material bore further rare earth elements such as dysprosium, samarium ...
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It is a colourless to pale yellow mineral with a vitreous luster. It has a tetragonal crystalline structure, and has the chemical makeup of Y(AsO₄), which is yttrium, arsenic, and oxygen, at a 1:1:4 ratio. It has a specific gravity of 4.866g/cm3. [1] Chernovite-(Y) is part of the Xenotime group.
Accessory minerals commonly observed in S-type granites include zircon, apatite, tourmaline, monazite and xenotime. Monazite is considered a diagnostic accessory mineral of S-type granites, whereas allanite is diagnostic of I-type granites. Oxide minerals in S-type granites will more commonly be ilmenite rather than magnetite. [1] [4]