Bustamite

Bustamite is a calcium manganese inosilicate (chain silicate) and a member of the wollastonite group. Magnesium, zinc and iron are common impurities substituting for manganese. Bustamite is the high-temperature polymorph of CaMnSi2O6 and johannsenite is the low temperature polymorph. The inversion takes place at 830 °C (1,530 °F), but may be very slow.
Bustamite could be confused with light-colored rhodonite or pyroxmangite, but both these minerals are biaxial (+) whereas bustamite is biaxial (−).

Bustamite
Bustamite (pink) with galena (grey) from Broken Hill, New South Wales, Australia. Specimen size 3.7 cm.
General
CategoryInosilicate
Formula
(repeating unit)
CaMn2+Si2O6
IMA symbolBst
Strunz classification9.DG.05 (10 ed)
8/F.18.40 (8 ed)
Dana classification65.2.1.2
Crystal systemTriclinic
Crystal classPinacoidal 1
(same H-M symbol)
Space groupI1
Identification
ColorLight pink to brownish red Pink color fades on exposure to sunlight
Crystal habitUsually tabular or equant to prismatic; commonly massive, often compact and fibrous
TwinningRare. Simple twins with (110) as the composition plane
Cleavage{100} perfect; {110} and {110} good; {010} poor
Mohs scale hardness5.5 to 6.5
LusterVitreous
StreakWhite
DiaphaneityTranslucent to transparent
Specific gravity3.32 to 3.43 (observed) 3.40 (calculated)
Optical propertiesBiaxial (−), 2V=34° to 60°
Refractive indexnα = 1.640 – 1.695, nβ = 1.651 – 1.708, nγ = 1.653 – 1.710
Birefringenceδ = 0.013 – 0.015
Dispersion r < v weak to strong
PleochroismWeak, X and Z orange, Y rose
SolubilityPartly soluble in HCl.
Other characteristicslattice: A B1
Specimens from the Franklin Mine are fluorescent red in longwave ultraviolet light. Not radioactive
References
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