Optical Properties
| Colour Pleochroism |
pale coloured in thin section with subtle pinkish to greenish pleochroism |
Form | euhedral crystals are usually stubby prisms, basal sections are 4 or 8 sided, with two primatic cleavages at 90° longitudinal sections are rectangular, exhibit one cleavage and parallel extinction |
| Relief RI |
moderate to high nalpha = 1.649-1.768 nbeta = 1.653-1.770 ngamma = 1.657-1.788 Generally increasing with increasing Fe content |
Cleavage | two good cleavages parallel to the {210} prism faces that intersect at 88° |
| Birefringence Interference Colours |
0.007-0.020 usually first order yellow or lower |
Twinning | rare |
| Interference Figure Optic Sign 2V |
Biaxial positive or negative 2VZ = 50-132° |
Optic Orientation | X=b, Y=a, Z=c optic plane parallel to (100) elongate fragments exhibit parallel extinction and are length slow |
| Composition | the effects of the substituion of Fe for Mg in orthopyroxene on the optical properties is evident in examining Figure 13.4 in Nesse. | Alteration | alters to serpentine, talc or fine grained amphibole |
| Occurrence | Mg-rich opx is common in mafic intrusive rocks (gabbro, norite, etc.). Fe-rich opx is found in more siliceous igneous rocks (diorite, syenite etc.). opx is common in high grade regional metamorphic rocks |
Distinguishing Features | distinguished from cpx by: 1) lower birefringence, 2) parallel extinction, 3) pale colour, weak pleochroism, 4) most common opx is optically negative, and 5) high 2V angle. |