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Formula | CaSiO3 | Pyroxenoid group. Usually pure, but Mn and Fe2+ can substitute for Ca. |
Crystal System | Triclinic | |
Crystal Habit | Columnar and fibrous elongate grains, often with twinning | |
Cleavage | Perfect cleavage on {100}, good cleavages on {001} and {-102} | Splitery cleavage fragments. Angles of cleavage: 84.5 degrees, and 70 degrees. |
Color/Pleochroism | Colorless, white, greyish, often with yellowish or brownish tint. Vitreous. No pleochroism | |
Optic Sign | Biaxial (-) | |
2Valpha | 36-60 degrees | Most wollastonite has a 2V of ~40º. This can be higher for Fe-bearing samples. |
Optic Orientation | X^c = -30 to -44 degrees Y^b ~ 0 degrees z^a = +35 to +49 degrees O.A.P. ~ (010) |
Cleavage fragments are length slow or length fast depending on orientation due to Y being parallel to fiber length. |
Refractive Indices
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alpha: 1.616-1.645 |
Increase with Fe and Mn content. |
Max Birefringence | 0.013-0.017 | Wollastonite resembles tremolite and pectolite, but both have a higher birefringence. |
Elongation | Grains elongate parallel to b | |
Extinction | Parallel | Elongate crystals display parallel extinction. |
Dispersion | r > v | |
Distinguishing Features | Colorless to grey in thin sectionwith moderate to moderatly high relief. First order interference color yellow-orange. One perfect cleavage and two good cleavages producing splintery cleavage fragments. H = 4.5-5. G = 2.86-3.09. Streak is colorless or white. | |
Occurrence | Occurs commonly as a product of contact and/or regional metamorphism in limestone and dolomite. Associated minerals include calcite, and grossular in hornfels, tremolite, epidote group members, diopside, and other Ca-Mg silicates. | |
Sources | Deer, W.A., Howie, R.A., Zussman, J. (1963) Rock-Forming Minerals, Chain Silicates, p. 94-100. Longmans, Green and Co LTD, London. |
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Editors | Sarah Martell (AC '06) , Carolyn Tewksbury ('07), Jessica Chang ('17) |
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Photomicrograph of wollastonite in plane and crossed polarized light (roll over image). Wollastonite has parallel extinction and has two good cleavages that intersect at an angle of 84º. |
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Photomicrograph of wollastonite in plane light (roll over image). Wollastonite typically has no color, and has distinct splintery cleavage in an end view. |
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Photomicrograph of wollastonite in plane and crossed polarized light showing elongated crystals having parallel extinction. |
WWW | Oxford University [images 74 and 75] |