Compare the texture with that of 121067. This lherzolite has a sheared or porphyroclastic texture. Both olivine and orthopyroxene show extreme effects of deformation. It is similar in many ways to the plagioclase lherzolite derived from oceanic lithosphere from Lherz. Compare this texture with that of 114282.
Olivine is colorless and has high relief in plane light.
Under crossed polars it has 2 to 3 interference colors. Grains of olivine may look twinned, due to sweeping extinction in which domains bounded by straight, boundaries are out of parallel by 1 or 2 . You might think that they are pieces broken off during shearing, but they are in fact grains of strain-free olivine nucleated and grown in an effort to relieve the strain in the larger crystal. The free energy of the strained crystal is lowered by recrystallization to an aggregate of smaller, strain-free grains. This process is called dynamic recrystallization and is an important aspect of strain recovery at high temperature.