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zircon

File:Zircon-dtn1a.jpg · Wikimedia Commons · See Wikimedia Commons

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Also known as zirconite, zirconium silicate

Zircon () is a mineral belonging to the group of nesosilicates and is a source of the metal zirconium. Its chemical name is zirconium(IV) silicate, and its corresponding chemical formula is ZrSiO4. An empirical formula showing some of the range of substitution in zircon is (Zr1–y, REEy)(SiO4)1–x(OH)4x–y. Zircon precipitates from silicate melts and has relatively high concentrations of high field strength incompatible elements. For example, hafnium is almost always present in quantities ranging from 1 to 4%. The crystal structure of zircon is tetragonal crystal system. The natural color of zirc

AI overview

Zircon is a mineral that contains zirconium metal and has the chemical formula ZrSiO4, making it an important source of zirconium for industrial use. It forms naturally from molten rock and is valued for its ability to concentrate certain rare elements, including hafnium, which are difficult to find in high concentrations elsewhere.

AI-generated from the Wikipedia summary — may contain errors.

Key facts

Mineral.caption
A lustrous crystal of zircon perched on a tan matrix of calcite from the Gilgit District of Pakistan
Mineral.formula
zirconium silicate 
Mineral.IMAsymbol
Zrn
Mineral.strunz
9.AD.30
Mineral.system
Tetragonal
Mineral.class
Ditetragonal dipyramidal (4/mmm) H-M symbol: (4/m 2/m 2/m)
Mineral.symmetry
I41/amd (No. 141)
Mineral.unit cell
a = 6.607(1), c = 5.982(1) [Å]; Z = 4
Mineral.color
Reddish brown, yellow, green, blue, gray, colorless; in thin section, colorless to pale brown
Mineral.boxbgcolor
b56042
Mineral.name
Zircon
Mineral.boxtextcolor
fff
Mineral.category
Nesosilicates
Mineral.image
Zircon-dtn1a.jpg
Mineral.imagesize
260px
Mineral.habit
tabular to prismatic crystals, irregular grains, massive
Mineral.twinning
On {101}. Crystals shocked by meteorite impact show polysynthetic twins on {112}
Mineral.cleavage
{110} and {111}

via Wikipedia infobox

Wikidata facts

Image
Zircon-t09zirc-06c.jpg
Show 8 more facts
Commons category
Zircon
chemical formula
ZrSiO₄
Nickel-Strunz 9th edition (updated 2009)
9.AD.30
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.AD.30
Mohs' hardness
7.5
density
4.65
IMA Mineral Symbol
Zrn
Strunz 8th edition (series ID, updated)
VIII/A.07
Sources (6)

via Wikidata · CC0

~13 min read

Article

11 sections
Contents
  • Properties
  • Applications
  • Gemstone
  • Occurrence
  • Radiometric dating
  • Similar minerals
  • Gallery
  • See also
  • References
  • Further reading
  • External links

{{Infobox mineral |boxbgcolor=#b56042| name = Zircon | boxtextcolor = #fff | category = Nesosilicates | image = Zircon-dtn1a.jpg | imagesize = 260px | caption = A lustrous crystal of zircon perched on a tan matrix of calcite from the Gilgit District of Pakistan | formula = zirconium silicate  | IMAsymbol = Zrn | molweight = | strunz = 9.AD.30 | system = Tetragonal | class = Ditetragonal dipyramidal (4/mmm) H-M symbol: (4/m 2/m 2/m) | symmetry = I41/amd (No. 141) | unit cell = a = 6.607(1), c = 5.982(1) [Å]; Z = 4 | color = Reddish brown, yellow, green, blue, gray, colorless; in thin section, colorless to pale brown | habit = tabular to prismatic crystals, irregular grains, massive | twinning = On {101}. Crystals shocked by meteorite impact show polysynthetic twins on {112} | cleavage = {110} and {111} | fracture = Conchoidal to uneven | tenacity = Brittle | mohs = 7.5 | luster = Vitreous to adamantine; greasy when metamict. | refractive = nω = 1.925–1.961 nε = 1.980–2.015, 1.75 when metamict | opticalprop = Uniaxial (+) | birefringence = δ = 0.047–0.055 | pleochroism = Weak | streak = White | gravity = 4.6–4.7 | melt = | fusibility = close to 2,550 °C depend on Hf,Th,U,H,etc... concentrations. | diagnostic = | solubility = Insoluble | diaphaneity = Transparent to opaque | other = Fluorescent and 25px radioactive,May form pleochroic halos,Relief: high | references = }}

Zircon () is a mineral belonging to the group of nesosilicates and is a source of the metal zirconium. Its chemical name is zirconium(IV) silicate, and its corresponding chemical formula is ZrSiO4. An empirical formula showing some of the range of substitution in zircon is (Zr1–y, REEy)(SiO4)1–x(OH)4x–y. Zircon precipitates from silicate melts and has relatively high concentrations of high field strength incompatible elements. For example, hafnium is almost always present in quantities ranging from 1 to 4%. The crystal structure of zircon is tetragonal crystal system. The natural color of zircon varies between colorless, yellow-golden, red, brown, blue, and green.

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