Smith College - Geology 222b - Petrology

Petrographic Data File

Omphacite
Property
Value
Comments
Formula

(Ca,Na)(Mg,Fe2+,Fe3+,Al)Si2O6

Crystal System monoclinic 2/m
Crystal Habit stubby crystals, most common as anhedral grains  
Cleavage good cleavage on {110}, intersect at 87 and 93° (similar to other pyroxenes), parting on {100} uneven to conchoidal fracture, brittle
Color/Pleochroism

Color in Hand Sample: green to dark green

Color in PPL: colorless to pale green

Pleochroism: weakly pleochroic, Z=very pale green to blue green

Optic Sign Biaxial (+)
2V 56-84° normal range for 2V= 60-75°
Refractive Index
 

alpha=1.662-1.701
beta=1.670-1.712
gamma=1.685-1.723

 
Distinguishing Features

High relief in thin section. Characteristic pyroxene cleavage. Gray streak. Hardness = 5-6.

Occurrence

Commonly found in rocks that formed in high-pressure conditions, such as eclogite, a high-pressure metamorphic/igneous rock. It is less commonly found in alpine metamorphic belts in blue schist, metagraywacke, and can also be found in granulites.

Editors Anna Lavarreda ('08j)

 
Photomicrograph of a mostly omphacite in plane polarized light. Click on the thumbnail to see a larger ppl/xpl rollover image.


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