Clinoptilolite (Na-K-)

Monoclinic  Images    

   
   
  Formula (Na,K,Ca0.5,Sr0.5,Ba0.5,Mg0.5)6Al6Si30O72 ∙ 20H2O
  Optic class & sign Biaxial positive or negative
  Optical orientation X = b, Y near a, Z near c
  Optical plane Optic plane ⊥ (010l)
  Relief Moderate-negative
  Refractive indices nx = 1.473 -1.491
ny = 1.475 -1.493
nz = 1.478 -1.497
n increases with CaAl substituting for NaSi
  Birefringence   (max.)0.003  - 0.006
   
  Optic Angle 2Vx = 85 - 90°
2Vz = 90 - 32°
  Sign of elongation Length-slow, l (+), for elongate cross-sections ⊥ (010), for the optical orientation shown; other indicatrix orientations show length-fast, I (-)
  Interference figure 
  Colour /   pleochroism Colourless
  Zoning -

  Form  Habit Platy
  Surface 
  Cleavage {010}
  Twinning Commonly not twinned
  Extinction Z∧c or trace of {100} = 18 – 23°; higher for K-Cpt

  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 n-Δn charts A, B: Bre - brewsterite, Cpt - clinoptilolite, Epi - epistilbite, Hul - heulandite,
Lev - levyne, Stb - stilbite, Yug - yugawaralite