Anhydrite

Anhydrite
Anhydrite
	Anhydrite, from Chihuahua, Mexico
General
Category	Sulfate mineral
Formula; (repeating unit)	CaSO4
IMA symbol	Anh
Strunz classification	7.AD.30
Dana classification	28.3.2.1
Crystal system	Orthorhombic
Crystal class	Dipyramidal (mmm) ; H–M symbol: (2/m 2/m 2/m)
Space group	Amma
Unit cell	a = 6.245(1) Å, b = 6.995(2) Å; c = 6.993(2) Å; Z = 4
Identification
Color	Colorless to pale blue or violet if transparent; white, mauve, rose, pale brown or gray from included impurities
Crystal habit	Rare tabular and prismatic crystals. Usually occurs as fibrous, parallel veins that break off into cleavage fragments. Also occurs as grainy, massive, or nodular masses
Twinning	Simple or repeatedly on {011} common; contact twins rare on {120}
Cleavage	[010] perfect; [100] perfect; [001] good, resulting in pseudocubic fragments
Fracture	Conchoidal
Tenacity	Brittle
Mohs scale hardness	3.5
Luster	Pearly on {010}; vitreous to greasy on {001}; vitreous on {100}
Streak	White
Diaphaneity	Transparent to translucent
Specific gravity	2.97
Optical properties	Biaxial (+)
Refractive index	nα = 1.567–1.574; nβ = 1.574–1.579; nγ = 1.609–1.618
Birefringence	δ = 0.042–0.044
Pleochroism	For violet varieties ; X = colorless to pale yellow or rose; Y = pale violet or rose; Z = violet.
2V angle	56–84°
Fusibility	2
Other characteristics	Some specimens fluoresce; many more fluoresce after heating
References

Anhydrite, or anhydrous calcium sulfate, is a mineral with the chemical formula CaSO₄. It is in the orthorhombic crystal system, with three directions of perfect cleavage parallel to the three planes of symmetry. It is not isomorphous with the orthorhombic barium (baryte) and strontium (celestine) sulfates, as might be expected from the chemical formulas. Distinctly developed crystals are somewhat rare, the mineral usually presenting the form of cleavage masses. The Mohs hardness is 3.5, and the specific gravity is 2.9. The color is white, sometimes greyish, bluish, or purple. On the best developed of the three cleavages, the lustre is pearly; on other surfaces it is glassy. When exposed to water, anhydrite readily transforms to the more commonly occurring gypsum, (CaSO₄·2H₂O) by the absorption of water. This transformation is reversible, with gypsum or calcium sulfate hemihydrate forming anhydrite by heating to around 200 °C (400 °F) under normal atmospheric conditions.^[6] Anhydrite is commonly associated with calcite, halite, and sulfides such as galena, chalcopyrite, molybdenite, and pyrite in vein deposits.

^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
^ Klein, Cornelis; Hurlbut, Cornelius S. (1985). Manual of Mineralogy (20th ed.). New York: John Wiley and Sons. ISBN 978-0-471-80580-9.
^ "Anhydrite". Webmineral.
^ "Anhydrite". Mindat.org.
^ "Anhydrite" (PDF). Handbook of Mineralogy.
^ Deer; Howie; Zussman (1992). An Introduction to the Rock=Forming Minerals (2nd ed.). England: Pearson Education. p. 614. ISBN 978-0-582-30094-1.

[1] Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.

[2] Klein, Cornelis; Hurlbut, Cornelius S. (1985). Manual of Mineralogy (20th ed.). New York: John Wiley and Sons. ISBN 978-0-471-80580-9.

[3] "Anhydrite". Webmineral.

[4] "Anhydrite". Mindat.org.

[5] "Anhydrite" (PDF). Handbook of Mineralogy.

[6] Deer; Howie; Zussman (1992). An Introduction to the Rock=Forming Minerals (2nd ed.). England: Pearson Education. p. 614. ISBN 978-0-582-30094-1.

[1]

[2]

[3]

[4]

[5]

[6]