Smith College - Geology 222b - Petrology

Petrographic Data File

Kyanite
Property
Value
Comments
Formula Al2SiO5 Fe+3, Ti+4, or Cr+3 may be subsituted.
Crystal System Triclinic  
Crystal Habit elongate crystals in bladed aggregates  
Cleavage Perfect cleavage on 100, good cleavage on 010  
Color/Pleochroism Pale blue in hand samples.  Colorless to light patchy blue in thin section.  Weak pleochroism in thin section where X= colorless, Y= light violet blue, and Z= light cobalt blue  Color may be streaky in hand samples.
Optic Sign Biaxial (-)  
2V 78-84

 

Optic Orientation Z: inclined 27° - 32° to the c axis
Y: inclined 27° - 32° to the b axis
X: inclined a few degrees to the a axis
Refractive Indices
alpha = 
beta = 
gamma = 
delta = 
1.710-1.718
1.719-1.725
1.724-1.734
0.012-0.016
 
Max Birefringence   usually not seen in grain mounts due to cleavages
Elongation    
Extinction Inclined (see optic orientation).  Bladed crystals display 0° - 30° extinction.
Dispersion    
Distinguishing Features Colorless and dark in thin section with high positive relief! Second-order interference colors. Two prominent, high angle cleavages occur parallel and perpendicular to the length of the crystal blades. Hardness = 4-5 parallel to c and 7.5 at right angles to c. G = 3.53 to 3.67. Streak is white.
Occurrence Commonly forms in rock types that have undergone high pressures. Kyanite is usually found in metamorphic rocks such as pelitic schists and gneisses. Infrequently found in kimberlite, granitic pegmatite, and eclogite. Associated minerals include staurolite, garnet, sillimanite, and andalusite.
Editors Wendy Kelly (05)

 
Photomicrograph of kyanite next to a garnet crystal and surrounded by muscovite in plane light. Kyanite typically displays pale green pleochroism and no distinct cleavage. Click on the image to see a larger image with xpl rollover.


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