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Thaumasite

Thaumasite (white) with prehnite (green) from Fairfax Quarry, Virginia
General
Category Mineral
Chemical formula Ca3Si(SO4)(CO3)(OH)6·12H2O
Identification
Molar mass 622.62 g/mol
Color Colorless, white
Crystal habit Prismatic, fibrous, massive, radial
Crystal system Hexagonal dipyramidal 6/m
Fracture Subconchoidal
Tenacity Brittle
Mohs scale hardness 3.5
Luster Vitreous to silky
Streak White
Diaphaneity Transparent to translucent
Specific gravity 1.877
Optical properties Uniaxial (-)
Refractive index nω = 1.498–1.507 nε = 1.458–1.470
Birefringence δ = 0.039

Thaumasite is a silicate mineral with chemical formula Ca3Si(CO3)(SO4)(OH)6·12(H2O). It occurs as colorless to white prismatic hexagonal crystals, typically as acicular radiating groups. It also occurs as fibrous masses. Its Mohs hardness is 3.5 and it has a specific gravity of 1.88 to 1.90. Optically it is uniaxial negative with indices of refraction of nω = 1.507 and nε = 1.468.

It occurs as a hydrothermal alteration mineral in sulfide ore deposits and geothermal alteration of basalt and tuff. It occurs with zeolites, apophyllite, analcime, calcite, gypsum and pyrite.

Thaumasite can also be formed along with other calcium-silicate hydrates (CSH) during cement alteration, especially when sulfate attack develops.

It was first described in 1878 in Sweden and named from the Greek, "thaumazein", to be surprised, in reference to its unusual composition with carbonate, sulfate and hydroxysilicate anions.

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