Mosandrite-(Ce)

mosandrite-(Ce)

eudialyte

rinkite

sodalite

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Formula: (Ca3REE)[(H2O)2Ca0.50.5]Ti(Si2O7)2(OH)2(H2O)2
Sorosilicate (Si2O7 groups), rinkite group of the seidozerite supergroup
Crystal System: Monoclinic
Specific gravity: 3.2 to 3.4 measured
Hardness: 4 to 5
Streak: Pale yellow, yellowish green
Colour: Deep reddish brown, brownish green, yellowish; greenish yellow
Solubility: Gelatinises with acids (Dana)
Weakly RADIOACTIVE
Environments:

Pegmatites

Mosandrite is an alteration product of rinkite (Dana).

At Mont Saint-Hilaire, Quebec, Canada, mosandrite occurs in eudialyte-rich pegmatites, sodalite xenoliths and nepheline syenite (Dana).

In Greenland mosandrite occurs in sodalite syenite (Dana).

The type locality is Låven, Larvik, Vestfold, Norway. Mosandrite-(Ce) specimens often shows signs of hydrothermal alteration. Here the alteration products may be a mixture of fluorite, pyrochlore, calcite, magnetite, pyrophanite and lorenzenite (Mindat).
Mosandrite-(Ce) has been found in many nepheline syenite pegmatites in Larvik, where it crystallised early in the paragenetic sequence. In most of the localities it has been subjected to hydrothermal alteration, leaving only traces of the original material. Alteration products are pyrophanite, magnetite, pyrochlore, fluorite, calcite, aegirine, titanite and lorenzenite. Most mosandrite-(Ce) samples are metamict, due to a small amount of thorium in the structure (JWW p161).

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