Omphacite

omphacite

chlorite

paragonite

ilmenite

Images

Formula: (Ca,Na)(Mg,Fe,Al)Si2O6
Inosilicate (chain silicate), single chains, clinopyroxene subgroup, pyroxene group

Jadeite, kosmochlor and omphacite are all members of the clinopyroxene subgroup, found in metamorphic environments, and components of Fei Cui (翡翠), the name preferred by modern gemmologists for "jade", which is a rock comprising intergrowths of the three minerals. The preferred terminology is "jadeite jade", "kosmochlor jade" and "omphacite jade" indicating the dominant mineral. NB "jade" is not synonymous with "jadeite". Nephrite is a rock composed mainly of amphiboles; it is not fei cui and preferably should not be referred to as jade.

Crystal System: Monoclinic
Specific gravity: 3.29 to 3.39
Hardness: 5 - 6
Streak: Greenish white
Colour: Dark green
Common impurities:Ti,Cr,Mn,K,H2O
Environments:

Metamorphic environments

Omphacite is an essential constituent of eclogite as a result of high pressure and high temperature metamorphism.
It is also found in kimberlites.
It is a characteristic mineral of the eclogite facies.

Alteration

amphibole, chlorite, paragonite, ilmenite, quartz and calcite to garnet, omphacite, rutile, H2O and CO2
NaCa2(Fe2Mg3)(AlSi7)O22(OH)2 + Mg5Al(AlSi3O10)(OH)8 + 3NaAl2(Si3Al)O10(OH)2 + 4Fe2+Ti4+O3 + 9SiO2 + 4CaCO3 → 2(CaMg2Fe3)Al4(SiO4)6 + 4NaCaMgAl(Si2O6)2 + 4TiO2 + 8H2O + 4CO2
In low-grade rocks relatively rich in calcite the garnet - omphacite association may be due to reactions such as the above (DHZ 2A p453).

amphibole, clinozoisite, chlorite, albite, ilmenite and quartz to garnet, omphacite, rutile and H2O
NaCa2(Fe2Mg3)(AlSi7)O22(OH)2 + 2Ca2Al3[Si2o7][SiO4]O(OH) + Mg5Al(AlSi3O10)(OH)8 + 3NaAlSi3O8 + 4Fe2+Ti4+O3 + 3SiO2 → 2(CaMg2Fe3)Al4(SiO4)6 + 4NaCaMgAl(Si2O6)2 + 4TiO2 + 6H2O
In low-grade rocks relatively poor in calcite the garnet - omphacite association may be developed by the above reaction (DHZ 2A p453).

augite, albite, pyroxene, anorthite and ilmenite to omphacite, garnet, quartz and rutile
2MgFe2+Si2O6 + Na(AlSi3O8) + Ca2Mg2Fe2+Fe3+AlSi5O18 + 2Ca(Al2Si2O8) + 2Fe2+Ti4+O3 → NaCa2MgFe2+Al(Si2O6)3 + (Ca2Mg3Fe2+4)(Fe3+Al5)(SiO4)9 + SiO2 + 2TiO2
This reaction occurs at high temperature and pressure (DHZ 2A p449).

diopside and albite to omphacite and quartz
CaMgSi2O6 + xNaAlSi3O8 ⇌ CaMgSi2O6.xNaAlSi2O6 + SiO2
(DHZ 2A p453)

labradorite, albite, forsterite and diopside to omphacite, garnet and quartz
3CaAl2Si2O8 + 2Na(AlSi3O8) + 3Mg2SiO4 + nCaMgSi2O6 → (2NaAlSi2O6 + nCaMgSi2O6) + 3(CaMg2)Al2(SiO4)3 + 2SiO2
(DHZ 2A p449)

Back to Minerals