Heulandite (Ca-)

Monoclinic  Images    

   
   
  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
ny = 1.487 -1.506
nz = 1.488 -1.512
n decreases with NaSi substituting for CaAl
  Birefringence   (max.)0.001  - 0.007
   
  Optic Angle 2Vx
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 -

  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)

  Reaction textures  
  Alteration /   decomposition 

  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 

  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