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Formula | (Ca0.5,Sr0.5,Ba0.5,Mg0.5,Na,K)9Al9Si27O72 ∙ 24H2O |
| Optic class & sign | Biaxial positive |
| Optical orientation | X near c, Y near a, Z = b |
| Optical plane | Optic plane ⊥ (010) |
| Relief | Moderate- to low-negative |
| Refractive indices | nx = 1.487 -1.505
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ny = 1.487 -1.506
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nz = 1.488 -1.512
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n decreases with NaSi substituting for CaAl |
| Birefringence (max.) | 0.001 - 0.007 |
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| Optic Angle
| 2Vx
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| 2Vz
= 35 - 75°; inconsistent values reported in literature (to 2V = 0) |
| Sign of elongation | Length-fast, l (-) in elongate sections of platy crystals |
| Interference figure | |
| Colour / pleochroism | Colourless |
| Zoning | - |
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Form | Habit | Tabular, granular |
| | Surface | |
| Cleavage | {010} |
| Twinning | Contact twins on {100} |
| Extinction | Straight in sections ⊥ (010); inclined in sections at a low angle to (010) |
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Reaction textures | |
| Alteration / decomposition | |
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Occurence | Ign | |
| | Met | Sediments incl pyroclastics at lowest-grade burial metamorphism, also from devitrification |
| | Sed | Diagenetic in submarine sediments, lake deposits |
| | Hyd | Cavities and veins in basalt, andesite and rhyolite |
| | Other | |
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Distinctive properties | Common zeolite. Very low n, very low to low Δn. Heulandite and clinoptilolite are difficult to distinguish from each other, but heulandite has commonly higher refractive indices. |
| Additional comments | Heating during preparation may change the optical properties of the more Si-rich members of the heulandite series to length-slow. n-Δn charts A, B: Bre - brewsterite, Cpt - clinoptilolite, Epi - epistilbite, Hul - heulandite, Lev - levyne, Stb - stilbite, Yug - yugawaralite |
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