Buddingtonite

Ammonium feldspar mineral From Wikipedia, the free encyclopedia

Buddingtonite is an ammonium feldspar with formula: NH4AlSi3O8 (note: some sources add 0.5H2O to the formula). It forms by hydrothermal alteration of primary feldspar minerals. It is an indicator of possible gold and silver deposits, as they can become concentrated by hydrothermal processes. It crystallizes in the monoclinic crystal system and is colorless to white with a vitreous luster. Its structure is analogous to that of high sanidine (KAlSi3O8). Buddingtonite has a hardness of 5.5 and a specific gravity of 2.32.

CategoryTectosilicate minerals
FormulaNH4AlSi3O8
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Buddingtonite
General
CategoryTectosilicate minerals
GroupFeldspar group
FormulaNH4AlSi3O8
IMA symbolBud[1]
IMA statusApproved (1964)
Strunz classification9.FA.30
Dana classification76.1.2.1
Crystal systemMonoclinic
Crystal classPrismatic (2)
or sphenoidal (2/m)
Space groupP21 (no. 4)
or C2/m (no. 12)
Unit cella = 8.57 Å, b = 13.03 Å,
c = 7.18 Å; β = 112.73°; Z = 4
Identification
ColorColorless
Crystal habitCompact masses replacing plagioclase as pseudomorphs
CleavageGood on {001}, distinct on {010}
TenacityBrittle
Mohs scale hardness5.5
LusterVitreous
StreakLight grey to yellow (impure specimens)
DiaphaneityTransparent to translucent
Specific gravity2.32
Optical propertiesBiaxial (+)
Refractive indexnα = 1.530 nβ = 1.531 nγ = 1.534
Birefringenceδ = 0.004
2V angleCalculated: 60°
References[2][3][4][5]
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Buddingtonite was discovered in 1964 at the Sulfur Bank mine near Clear Lake in Lake County, California.[6] Clear Lake is at the north end of The Geysers geothermal area. It also occurs in the Tonopah, Nevada[7] area and in hydrothermal areas in New Zealand[8] and Japan. It has also been reported from the sedimentary Phosphoria Formation in Idaho,[9] South Dakota,[10] Wyoming, and Montana. It occurs in the oil shale deposit, near Proserpine, Queensland, Australia.[11]

It was named for Arthur Francis Buddington (1890–1980), a petrologist at Princeton University.

References

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