Formula: Mg9(SiO4)4(OH)2
Nesosilicate (insular SiO4 groups), humite subgroup,
humite group
Crystal System: Monoclinic
Specific gravity: 3.13 measured, 3.14 calculated
Hardness: 6½
Streak: White
Colour: Pale yellow to orange-yellow, almost colourless
Environments:
Hydroxylclinohumite occurs in skarn rims around
dolomitic marble xenoliths in
gabbroic rocks.
Alteration
diopside, dolomite and
H2O ⇌ hydroxylclinohumite,
calcite and CO2
2CaMgSi2O6 + 7CaMg(CO3)2 + H2O ⇌
Mg9(SiO4)4(OH)2 + 9CaCO3 + 5CO2
In the nodular dolomites, hydroxylclinohumite
associated with
calcite occurs in a narrow zone in the central parts of the
nodules due to the above reaction
(DHZ 1A p264).
forsterite, dolomite and H2O to
calcite, hydroxylclinohumite
and CO2
4Mg2SiO4 + CaMg(CO3)2 + H2O →
Mg9(SiO4)4(OH)2 +CaCO3 + CO2
A forsterite-clinohumite assemblage in the silica-rich
dolomite in the aureole of the Alta
granodiorite in Utah, USA, is
probably due to the above reaction
(DHZ 1A p264).
tremolite, dolomite and
H2O ⇆
hydroxylclinohumite, calcite
and CO2
Ca2Mg5Si8O22(OH)2 + 13CaMg(CO3)2
+ H2O ⇆ 2Mg9(SiO4)4(OH)2 + 15CaCO3 + 11CO2
(DHZ 1A p264).
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