Clinopyroxene
Mineral Name
|
Diopside
|
Augite
|
Pigeonite
|
Crystal System
|
Monoclinic |
Monoclinic |
Monoclinic |
Chemical Comp..
|
CaMgSi2O6 |
(CaNa,Mg,Fe,Al,Ti)2Si2O6 |
(Mg,Fe,Ca)2Si2O6
|
Color
|
Colorless
|
Colorless/Pale Green |
Colorless
|
Pleochroism
|
None
|
Weak Brown-Green |
None/Weak Yellow
|
Cleavage
|
2@90˚
in basal
|
2@90˚
in basal |
2@90˚ in basal
|
Relief
|
Moderate |
Moderate
|
Moderate
|
Birefringence
|
High 1st/Low 2nd
Order |
High 1st/Low 2nd
Order
|
Moderate-High 1st Order
|
2V |
38˚-48˚
|
25˚-83˚
|
0˚-30˚
|
Optic Sign |
Positive |
Positive |
Positive
|
Twinning
|
Simple & Multiple |
Simple & Multiple
|
Simple or Lamellar
|
The top two photomicrographs show the
weak pale green pleochroism of Clinopyroxene. The bottom
photomicrograph shows that even though the cleavage planes are vertical
(aligned N-S), the crystal is still in illumination under cross
polarized light.
Series of photomicrographs showing the weak pleochroism of
Clinopyroxene (top two photomicrographs, taken in plane polarized
light). The bottom photomicrograph (taken in cross polarized light)
demonstrates the higher birefringence of Clinopyroxene compared to
Orthopyroxene, as well as the fact that it does not exhibit straight
extinction.