Formula: ☐Fe2+2Fe2+5Si8O22(OH)2
Inosilicate (chain silicate),
magnesium-iron-manganese amphibole subgroup,
amphibole supergroup
Crystal System: Monoclinic
Specific gravity: 3.4 to 3.5
Hardness: 5 to 6
Streak: Colourless
Colour: Ashen, brown, brownish green, dark gray
Environments:
Grunerite is common in iron formations due to medium to high grade
contact metamorphism, and it also occurs in some
blueschist facies
quartzite.
Upon further metamorphism cummingtonite and grunerite give way to
orthopyroxene or olivine.
Alteration
cummingtonite-grunerite and H2O to
serpentine and quartz
6(Fe,Mg)7Si8O22(OH)2 + 22H2O ⇌
7(Fe,Mg)6Si4O10(OH)8 + 20SiO2
(DHZ 2A p138)
cummingtonite-grunerite and olivine to
enstatite-ferrosilite and
H2O
(Fe,Mg)7Si8O22(OH)2 + (Mg,Fe)2SiO4 ⇌
9(Mg,Fe2+)SiO3 + H2O
(DHZ 2A p138)
enstatite-ferrosilite,
SiO2 and H2O to
cummingtonite-grunerite
7(Mg,Fe2+)SiO3 + SiO2 + H2O ⇌
(Fe,Mg)7Si8O22(OH)2
(DHZ 2A p138)
fayalite, SiO2 and H2O
to grunerite
7Fe2+2(SiO4) + 9SiO2 + 2H2O
→ 2Fe2+2Fe2+5Si8O22(OH)2
Fayalite may undergo partial regression to grunerite according to the above
reaction.
(DHZ 1A p265)
ferro-actinolite to
hedenbergite,
grunerite, quartz and H2O
7Ca2Fe2+5Si8O22(OH)2 →
14CaFe2+Si2O6 +
3Fe2+2Fe2+5 Si8O22(OH)2 +
4SiO2 + 4H2O
In some calc-silicate rocks hedenbergite is the product of metamorphism of
iron-rich sediments, probably due to the instability of ferro-actinolite with
rising temperature. The association of
hedenbergite and
grunerite has been widely described, and its formation may be due to the
above reaction
(DHZ 2A p273).
greenalite to grunerite, fayalite
and H2O
9Fe3Si2O5(OH)4 →
Fe2+2Fe2+5Si8O22(OH)2 +
10Fe2SiO4 + 17H2O
CM 36.157).
greenalite and minnesotaite to
grunerite and H2O
2Fe3Si2O5(OH)4 +
5Fe2+3Si4O10(OH)2 →
3Fe2+2Fe2+5Si8O22(OH)2 + 6H2O
CM 36.157).
Mg-rich greenalite to olivine,
grunerite and H2O
18(Fe2+, Mg))3Si2O5(OH)4 →
20(Fe,Mg)2SiO4 + 2(Fe2+,Mg)7Si8O22(OH)2
+ 34H2O
(DHZ 1A p266)
minnesotaite to grunerite,
SiO2 and H2O
7Fe2+3Si4O10(OH)2 →
3Fe2+2Fe2+5Si8O22(OH)2 +
4SiO2 + 4H2O
CM 36.157).
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