Carpholite

Orthorhombic  Images    

   
   
  Formula (Mn,Mg,Fe)Al2Si2O6(OH)4
  Optic class & sign Biaxial negative
  Optical orientation X = b, Y = a, Z = c
  Optical plane (100)
  Relief Moderate-positive
  Refractive indices nx = 1.611 -1.628
ny = 1.627 -1.644
nz = 1.630 -1.647
n increases with Fe
  Birefringence   (max.)0.019  - 0.022
   -
  Optic Angle 2Vx = 50 - 87°
2Vz
  Sign of elongation Length-slow, l (+)
  Interference figure 
  Colour /   pleochroism X: pale yellow to greenish; Y: pale yellow Z: colourless or pale blueish to blueish green; absorption X ≥ Y > Z
  Zoning 

  Form  Habit Acicular, fibrous, radiating aggregates
  Surface Subhedral to anhedral
  Cleavage {010} perfect; (110) indistinct, at 68 and 112°
  Twinning {100}
  Extinction Straight to cleavages and {110} faces in sections ∥ c; straight to {010} cleavage and symmetrical to (110) cleavage and faces in sections orthogonal to c

  Reaction textures  
  Alteration /   decomposition Chlorite, sudoite

  Occurence     Ign 
  Met Low-grade metamorphic phyllites and schists; ferrocarpholite and magnesiocarpholite are restricted in their occurrence to low-temperature, high-pressure rocks (> 7 bar), Mn-carpholite to low pressures.
  Sed 
  Hyd Quartz veins
  Other 

  Distinctive   properties               Habit, pleochroism, occurrence; straw-yellow colour in hand specimen
  Additional   comments Optical data on Mg-carpholite are poor; refractive indices may be somewhat lower than those given above (1.58 – 1.60).