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Formula | (Na,Ca,K)6-8(AlSiO4)6(CO3,SO4,Cl,OH)1-2 ∙ 1-5H2O |
| Optic class & sign | Uniaxial negative |
| Relief | Moderate to low negative |
| Refractive indices | no = 1.490 -1.530
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ne = 1.488 -1.503
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n decreases with increasing Na and SO42- substitution for Ca and CO32- |
| Birefringence (max.) | 0.002 - 0.028 |
| | Δn decreases with increasing Na and SO42- substitution for Ca and CO32- |
| Sign of elongation | Length-fast, l (-) |
| Interference figure | |
| Colour / pleochroism | Colourless |
| Zoning | |
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Form | Habit | Short-prismatic to granular |
| | Surface | Commonly subhedral to anhedral |
| Cleavage | 3 sets, {1010} perfect; {0001} poor |
| Twinning | Rare lamellar twins |
| Extinction | Straight with respect to prism faces and {1010} cleavage in sections ∥ c |
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Reaction textures | Breakdown product of nepheline; reaction zones between nepheline and calcite |
| Alteration / decomposition | Replacement by calcite |
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Occurence | Ign | Nepheline syenites and related alkaline rocks |
| | Met | |
| | Sed | |
| | Hyd | |
| | Other | |
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Distinctive properties | Negative relief; Ca-CO3-rich cancrinite shows distinctly higher Δn than nepheline or feldspar |
| Additional comments | Cl-rich cancrinite (microsommite) is optically positive |
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