Carletonite
{{Short description|Silicate mineral}}
{{Infobox mineral
| name = Carletonite
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| image = Carletonite-20263.jpg
| imagesize = 280px
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| caption = Carletonite, Poudrette quarry, Mont Saint-Hilaire, Montérégie, Quebec, Canada
| category = Phyllosilicate
| formula = KNa4Ca4(CO3)4Si8O18(F,OH)·(H2O)
| molweight =
| strunz = 9.EB.20
| system = Tetragonal
| class = Ditetragonal dipyramidal (4/mmm)
H–M symbol: (4/m 2/m 2/m)
| symmetry = P4/mbm
| unit cell = a = 13.17 Å, c = 16.69 Å; Z = 4
| colour = Colourless, light blue, dark blue, or pink
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| habit = Prismatic crystals, massive
| twinning =
| cleavage = Perfect on {001}, good on {110}
| fracture = Conchoidal
| tenacity = Brittle
| mohs = 4 - {{frac|4|1|2}}
| lustre = Vitreous
| streak = White
| diaphaneity = Transparent to translucent
| gravity = 2.45
| density =
| polish =
| opticalprop = Uniaxial (-)
| refractive = nω = 1.521 nε = 1.517
| birefringence = δ = 0.004
| pleochroism = Weak; O = pale blue; E = pale pinkish brown
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| references = [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Carletonite Mineralienatlas][http://rruff.geo.arizona.edu/doclib/hom/carletonite.pdf Handbook of Mineralogy][http://www.mindat.org/min-898.html Mindat.org][http://webmineral.com/data/Carletonite.shtml Webmineral data]
}}
Carletonite is a rare silicate mineral with formula KNa4Ca4(CO3)4Si8O18(F,OH)·(H2O).
It is a phyllosilicate and a member of the apophyllite group. Its tetragonal crystals are a translucent blue, white, colorless or pink with a vitreous to dull lustre. It has a density of 2.45 and a hardness of 4–4.5.
It was discovered by G.Y Chao and named for the school he attended, Carleton University of Ottawa.[http://www.reciprocalnet.org/recipnet/showsamplebasic.jsp?sampleId=27344235 Carletonite is a rare mineral found only in Mt Saint-Hilaire, Quebec, Canada.] It was first described in 1969 for an occurrence at Mont Saint-Hilaire, Quebec. The type locality at Mont Saint–Hilaire is the only reported occurrence.
It occurs in hornfels and siliceous marble xenoliths within and adjacent to a nepheline syenite intrusion. It occurs in association with quartz, narsarsukite, calcite, fluorite, ancylite, molybdenite, leucosphenite, lorenzenite, galena, albite, pectolite, apophyllite, leifite, microcline and arfvedsonite.