Sanidine

Monoclinic  Images    

   
   
  Formula (K,Na)AlSi3O8
  Optic class & sign Biaxial negative
  Optical orientation a near X, b = Z, c near Z
  Optical plane Low-sanidine: orthogonal to (010); high-sanidine: ∥ (010)
  Relief Low negative
  Refractive indices nx = 1.518 -1.527
ny = 1.522 -1.532
nz = 1.522 -1.534
n increases with increasing Ab component
  Birefringence   (max.)0.005  - 0.007
   Δn increases with increasing Ab component. Crystals commonly unzoned.
  Optic Angle 2Vx = 0 - 60° for low-sanidine, 0 - 60° for high-sanidine
2Vz
  Sign of elongation Length-fast, l (-) for crystals elongate ∥ a
  Interference figure Diffuse isogyres on a white background; 2V is controlled by the degree of disorder as well as composition. Distinction between low- and high-sanidine requires recognition of the (010) plane in the form of a twin plane or crystal face. Obtain optic axis figure and check OP orientation against (010) in orthoscopic image.
  Colour /   pleochroism Colourless
  Zoning 

  Form  Habit Tabular; acicular in spherulites in volcanic glass
  Surface Euhedral phenocrysts in volcanics
  Cleavage {001} perfect, {010} distinct, orthogonal to each other
  Twinning {010} Carlsbad twins most common
  Extinction Inclined, up to 5° to {001} cleavage traces

  Reaction textures  
  Alteration /   decomposition Kaolinite, illite, sericite

  Occurence     Ign Silicic volcanic and sub-volcanic rocks
  Met Xenoliths in lavas or dykes; high-temperature, low-pressure contact zones (sanidinite facies)
  Sed 
  Hyd 
  Other 

  Distinctive   properties               Low n, low Δn, characteristic twinning, occurrence; distinction between high- and low-sanidine see under ‘Interference figure’.
  Additional   comments Preservation of high-sanidine (disordered structure) requires rapid quenching. The division between high-sanidine and low-sanidine is set at 2V = 0, where the OP orientation switches.
The diagram below shows the relationship between 2Vx, composition and Al-Si order/disorder for alkalifeldspars.