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EntityQ420801· pop 17· linked from 10 articles

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 , 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 (−).

Key facts

Mineral.name
Bustamite
Mineral.category
Inosilicate
Mineral.image
Bustamite.jpg
Mineral.caption
Bustamite (pink) with galena (grey) from Broken Hill, New South Wales, Australia. Specimen size 3.7 cm.
Mineral.formula
CaMn2+Si2O6
Mineral.IMAsymbol
Bst
Mineral.strunz
9.DG.05 (10 ed) 8/F.18.40 (8 ed)
Mineral.dana
65.2.1.2
Mineral.system
Triclinic
Mineral.class
Pinacoidal (same H-M symbol)
Mineral.symmetry
I
Mineral.color
Light pink to brownish red Pink color fades on exposure to sunlight
Mineral.habit
Usually tabular or equant to prismatic; commonly massive, often compact and fibrous
Mineral.twinning
Rare. Simple twins with (110) as the composition plane
Mineral.cleavage
{100} perfect; {110} and {10} good; {010} poor
Mineral.mohs
5.5 to 6.5
Mineral.luster
Vitreous
Mineral.refractive
nα = 1.640 – 1.695, nβ = 1.651 – 1.708, nγ = 1.653 – 1.710

via Wikipedia infobox

Wikidata facts

Image
Bustamite-351345.jpg
Show 6 more facts
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.DG.05
Commons category
Bustamite
Nickel-Strunz 9th edition (updated 2009)
9.DG.05
IMA Mineral Symbol
Bst
chemical formula
CaMn²⁺(Si₂O₆)
Strunz 8th edition (series ID, updated)
VIII/D.08a
Sources (1)

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Article

5 sections
Contents
  • Cell parameters
  • Type locality
  • Environment
  • References
  • External links

{{Infobox mineral | name = Bustamite | category = Inosilicate | image = Bustamite.jpg | imagesize = | caption = Bustamite (pink) with galena (grey) from Broken Hill, New South Wales, Australia. Specimen size 3.7 cm. | formula = CaMn2+Si2O6 | IMAsymbol=Bst | molweight = | strunz = 9.DG.05 (10 ed) 8/F.18.40 (8 ed) | dana = 65.2.1.2 | system = Triclinic | class = Pinacoidal (same H-M symbol) | symmetry = I | color = Light pink to brownish red Pink color fades on exposure to sunlight | habit = Usually tabular or equant to prismatic; commonly massive, often compact and fibrous | twinning = Rare. Simple twins with (110) as the composition plane | cleavage = {100} perfect; {110} and {10} good; {010} poor | fracture = | tenacity = | mohs = 5.5 to 6.5 | luster = Vitreous | refractive = nα = 1.640 – 1.695, nβ = 1.651 – 1.708, nγ = 1.653 – 1.710 | opticalprop = Biaxial (−), 2V=34° to 60° | birefringence = δ = 0.013 – 0.015 Dispersion r Specimens from the Franklin Mine are fluorescent red in longwave ultraviolet light. Not radioactive | references = }} 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 , 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 (−).

==Cell parameters== There is considerable variety in the literature about the size and type of the unit cell, the formula to be used, and the value of Z, the number of formula units per unit cell.

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