Spurrite

Spurrite
Spurrite
	Spurrite from New Mexico
General
Category	Nesosilicate
Formula; (repeating unit)	Ca5(SiO4)2CO3
IMA symbol	Spu[1]
Strunz classification	9.AH.15
Crystal system	Monoclinic
Crystal class	Prismatic (2/m) ; (same H-M symbol)
Space group	P21/a
Identification
Color	Gray, gray white to lilac gray
Crystal habit	Massive to granular
Twinning	Polysynthetic twins on [001] and [101]
Cleavage	Distinct on [100]
Fracture	Uneven to splintery
Mohs scale hardness	5
Luster	vitreous to resinous
Streak	White
Diaphaneity	Transparent to translucent
Specific gravity	3
Optical properties	Biaxial (-)
Refractive index	nα = 1.640–1.641 nβ = 1.674–1.676 nγ = 1.679–1.681
Birefringence	δ = 0.039–0.040
Other characteristics	Green cathodoluminescence
References	[2][3][4]

Spurrite is a white, yellow or light blue mineral with monoclinic crystals. Its chemical formula is Ca₅(Si O₄)₂CO₃.[5]

Spurrite is generally formed in contact metamorphism zones as mafic magmas are intruded into carbonate rocks.[6] Spurrite's space group is P 2/a. It is biaxial with a birefringence of 0.0390–0.0400, giving second order red interference colors when viewed under crossed polarizers in a petrographic microscope.[7]

The calcium is in six-fold coordination with the oxygen, the silicon is in a four-fold coordination with the oxygen and the carbon is in two-fold coordination. One unique characteristic of spurrite is that it actually abides by two twin laws. Polysynthetic twinning can occur along its (001) and another type of twinning can occur parallel to its optical axes.[6]

Discovery and occurrence

Spurrite was first described in 1908 for an occurrence in the Terneras Mine, Velardeña District, Durango, Mexico. It was named for American economic geologist Josiah Edward Spurr (1870–1950).[3]

In addition to its type locality, spurrite has been reported from Riverside County, California; Luna County, New Mexico; and from the Little Belt Mountains, Lewis and Clark County, Montana. It is also found in Ireland, Scotland, New Zealand, Turkey, Israel, Japan and Siberia.[2]

Cement manufacture contaminant

Spurrite forms as contaminating spurrite rings on the walls of cement kilns during the production of Portland cement.[8]

References

Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. doi:10.1180/mgm.2021.43. S2CID 235729616.
http://rruff.geo.arizona.edu/doclib/hom/spurrite.pdf Mineral Handbook
http://www.mindat.org/min-3734.html Mindat
http://webmineral.com/data/Spurrite.shtml Webmineral data
Richard V. Gaines, H. Catherine W. Skinner, Eugene E. Foord, Brian Mason, and Abraham Rosenzweig: Dana's new mineralogy, p. 1106. John Wiley & Sons, 1997
Smith, J.V. (1960) "The Crystal structure of Spurrite, Ca₅(SiO₄)₂CO₃". Acta. Cryst. 13, 454
Barthemy, D. (2000) Afwillite Mineral Data, (http://webmineral.com/data/Afwillite.shtml)
Mosci, Ricardo, 1998, How To Eliminate Calcining Zone Rings, Cement America http://cementamericas.com/mag/cement_eliminate_calcining_zone/

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

[Handbook-2] ttp://rruff.geo.arizona.edu/doclib/hom/spurrite.pdf Mineral Handbook

[Mindat-3] ttp://www.mindat.org/min-3734.html Mindat

[4] ttp://webmineral.com/data/Spurrite.shtml Webmineral data

[5] Richard V. Gaines, H. Catherine W. Skinner, Eugene E. Foord, Brian Mason, and Abraham Rosenzweig: Dana's new mineralogy, p. 1106. John Wiley & Sons, 1997

[Smith-6] Smith, J.V. (1960) "The Crystal structure of Spurrite, Ca₅(SiO₄)₂CO₃". Acta. Cryst. 13, 454

[7] Barthemy, D. (2000) Afwillite Mineral Data, (http://webmineral.com/data/Afwillite.shtml)

[8] Mosci, Ricardo, 1998, How To Eliminate Calcining Zone Rings, Cement America http://cementamericas.com/mag/cement_eliminate_calcining_zone/