Omphacite | |
---|---|
General | |
Category | Pyroxene |
Formula (repeating unit) | (Ca,Na)(Mg,Fe2+,Al)Si2O6 |
IMA symbol | Omp[1] |
Strunz classification | 9.DA.20 |
Dana classification | 65.01.03b.01 (clinopyroxene) |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P2/n or C2/c |
Unit cell | a = 9.66, b = 8.81, c = 5.22 [Å]; β = 106.56°; Z = 4 |
Identification | |
Color | Green to dark green; colorless to pale green in thin section |
Crystal habit | Rarely in rough crystals; anhedral, granular to massive |
Twinning | Single and polysynthetic twinning common on {100} |
Cleavage | Good on {110}, {110} ^ {110} ≈87°; parting on {100} |
Fracture | Uneven to conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 5–6 |
Luster | Vitreous to silky |
Streak | Greenish white |
Diaphaneity | Translucent |
Specific gravity | 3.16–3.43 |
Optical properties | Biaxial (+) |
Refractive index | nα = 1.662 – 1.701 nβ = 1.670 – 1.712 nγ = 1.685 – 1.723 |
Birefringence | δ = 0.023 |
Pleochroism | Weak; X = colorless; Y = very pale green; Z = very pale green, blue-green |
2V angle | Measured: 58° to 83°, Calculated: 74° to 88° |
References | [2][3][4][5] |
Omphacite is a member of the clinopyroxene group of silicate minerals with formula: (Ca, Na)(Mg, Fe2+, Al)Si2O6. It is a variably deep to pale green or nearly colorless variety of clinopyroxene. It normally appears in eclogite, which is the high-pressure metamorphic rock of basalt. Omphacite is the solid solution of Fe-bearing diopside and jadeite.[6] It crystallizes in the monoclinic system with prismatic, typically twinned forms, though usually anhedral. Its space group can be P2/n or C2/c depending on the thermal history.[7] It exhibits the typical near 90° pyroxene cleavage. It is brittle with specific gravity of 3.29 to 3.39 and a Mohs hardness of 5 to 6.