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EntityQ517231· pop 12· linked from 10 articles

Also known as IMA1974-018

Hafnon is a hafnium nesosilicate mineral with the idealized chemical formula . It is the mineral form of hafnium silicate and one of the few known minerals with essential hafnium.

Key facts

Mineral.name
Hafnon
Mineral.image
Hafnon.jpg
Mineral.caption
Very small brown single crystals of hafnon from Bernic Lake, Lac-du-Bonnet District, Manitoba, Canada
Mineral.category
Nesosilicates
Mineral.IMAsymbol
Haf
Mineral.strunz
09.AD.30
Mineral.system
Tetragonal
Mineral.dana
51.05.02.02
Mineral.class
Ditetragonal Dipyramidal (4/mmm ) H-M symbol: (4/m 2/m 2/m)
Mineral.symmetry
I41/amd
Mineral.unit cell
a = 6.5725(7) Å, c = 5.9632(4) Å=; Z = 4
Mineral.habit
Euhedral to irregular crystals
Mineral.cleavage
{???} Indistinct
Mineral.mohs
7.5
Mineral.luster
Vitreous
Mineral.opticalprop
Uniaxial (+)
Mineral.refractive
nω = 1.930 - 1.970 nε = 1.980 - 2.030
Mineral.birefringence
δ = 0.050

via Wikipedia infobox

~2 min read

Encyclopedic overview

2 sections
Contents
  • Chemistry
  • References

{{Infobox mineral |name=Hafnon |image=Hafnon.jpg |caption=Very small brown single crystals of hafnon from Bernic Lake, Lac-du-Bonnet District, Manitoba, Canada |category=Nesosilicates |formula= | IMAsymbol = Haf|strunz=09.AD.30|system=Tetragonal|dana=51.05.02.02|class=Ditetragonal Dipyramidal (4/mmm ) H-M symbol: (4/m 2/m 2/m)|symmetry=I41/amd|unit cell=a = 6.5725(7) Å, c = 5.9632(4) Å=; Z = 4|habit=Euhedral to irregular crystals|cleavage={???} Indistinct|mohs=7.5|luster=Vitreous|opticalprop=Uniaxial (+)|refractive=nω = 1.930 - 1.970 nε = 1.980 - 2.030|birefringence=δ = 0.050|streak=grey white|density=6.97|diaphaneity=Transparent|impurities=Often zoned with zircon. Forms part of zircon-hafnon series|colour=Orange-red,brownish yellow, rarely colourless}}

Hafnon is a hafnium nesosilicate mineral with the idealized chemical formula . It is the mineral form of hafnium silicate and one of the few known minerals with essential hafnium.

Excerpted from Wikipedia’s “hafnon” article, available under the CC BY-SA 4.0 licence.

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